americanmalacologists, inc.
PUBLISHERS OF DISTINCTIVE BOOKS ON MOLLUSKS
THE NAUTILUS (Quarterly)
MONOGRAPHS OF MARINE MOLLUSCA
STANDARD CATALOG OF SHELLS
INDEXES TO THE NAUTILUS
{Geographical, vols 1-90; Scientific Names, vols 61-90)
REGISTER OF AMERICAN MALACOLOGISTS
JANUARY 31, 1986
THE
NAUTILUS
FEB 5 1986
I Woods Hole, Mass.
ISSN 0028-1344
Vol. 100
No. 1
A quarterly
devoted to
malacology and
the interests of
conchologists
Founded 1889 by Henry A. Pilsbry. Continued by H. Burrington Baker.
Editor-in-Chief: R. Tucker Abbott
EDITORIAL COMMITTEE
CONSULTING EDITORS
Dr. William K. Emerson
Department of Living Invertebrates
The American Museum of Natural History
New York, NY 10024
Mr. Samuel L. B. Fuller
1053 Mapleton Avenue
Suffield, CT 06078
Dr. M. G. Harasewych
363 Crescendo Way
Silver Spring, MD 20901
Mr. Richard I. Johnson
Department of Mollusks
Museum of Comparative Zoology
Cambridge, MA 02138
Dr. Aurele La Rocque
Department of Geology
The Ohio State University
Columbus, OH 43210
Dr. James H. McLean
Los Angeles County Museum of Natural History
900 Exposition Boulevard
Los Angeles, CA 90007
Dr. Arthur S. Merrill
c/o Department of Mollusks
Museum of Comparative Zoology
Cambridge, MA 02138
Dr. Donald R. Moore
Division of Marine Geology
School of Marine and Atmospheric Science
10 Rickenbacker Causeway
Miami, FL 33149
Dr. G. Alan Solem
Department of Invertebrates
Field Museum of Natural History
Chicago, IL 60605
Dr. David H. Stansbery
Museum of Zoology
The Ohio State University
Columbus, OH 43210
Dr. Ruth D. Turner
Department of Mollusks
Museum of Comparative Zoology
Cambridge, MA 02138
Dr. Gilbert L. Voss
Division of Biology
School of Marine and Atmospheric Science
10 Rickenbacker Causeway
Miami, FL 33149
EDITOR-IN-CHIEF
Dr. R. Tucker Abbott
American Malacologists, Inc.
Box 2255, Melbourne, FL 32902-2255
Mrs. Cecelia W. Abbott
Business and Subscription Manager
P.O. Box 2255
Melbourne, FL 32902-2255
Second Class Postage paid at Melbourne, Florida
and other post offices
The Nautilus (USPS 374-980)
ISSN 0028-1344
A quarterly magazine devoted to malacology.
Copyright ^1986 by American Malacologists, Inc.
OFFICE OF PUBLICATION
American Malacologists, Inc. (United Parcel Address:
2208 South Colonial Drive, Melbourne, FL 32901)
Mail: Box 2255, Melbourne, FL 32902-2255
POSTMASTER: Send address changes to above.
Subscription Price: $15.00 (see inside back cover)
$17.00 (foreign); institutions $20.00
THE
NAUTILUS
Volume 100, number 1 — January 31, 1986
ISSN 0028-1344
CONTENTS
Dedication of the 100th Volume 1
Birth and Growth of The Nautilus 2
Tom Pullev and the Train 8
Joseph Rosewater (1928-1985)
A Tribute and Bibliography by Harald A. Rehder .
Andrew C. Miller, Barry S. Payne and Terry Siemsen
Description of the Habitat of the Endangered Mussel Plethobasus cooperianus 14
Andrew C. Miller, Barry S. Payne and David W. Aldridge
Characterization of a Bivalve Community in the Tangipahoa River, Mississippi 18
Richard A. Petit
Notes on Species of Brocchinia (Gastropoda: Cancellariidae) 23
William K. Emerson
On the Type Species oi Metula H. & A. Adams, 1853:
Buccinum. clathratum A. Adams and Reeve, 1850 (Gastropoda: Buccinidae) 27
Eugene Coan
Some Additional Taxonomic Units that First Appear in Publications by J. G. Cooper 30
Dee S. Dundee
Notes on the Habits and Anatomy of the Introduced Land Snails,
Rumina and Lamellaxis (Subulinidae) 32
Award News 37 Notes; Deaths 38
STATEMENT OF OWNERSHIP, MANAGEMENT AND CIRCULA-
TION (Required by) Act of October 23, 1962: Section 4396, Title
39. United States Code, and postal regulation 132-622.
1. Title of publication THE NAUTILUS.
2. Date of filing: September 14, 1985
3. Frequency of Issue: Quarterly (4 per year).
4. Location of known office of publication: 2208 South
Colonial Dr., Melbourne, FL 32901.
5. Location of Headquarters of General Business Offices
of the Publishers: 2208 South Colonial Dr., Melbourne, FL
32901 ,
6. Names and addresses of publisher, editor, and manag-
ing editor: Publisher, American Molocologists, Inc., P.O.
Box 2255, Melbourne, FL 32901, Editor, R. Tucker Abbott,
P.O. Box 2255, Melbourne, FL 32902, Business Manager,
Mrs. Cecelia W Abbott, P.O, Box 2255, Melbourne, FL
32902-2255,
7. Owner: American Molocologists, Inc., P.O. Box 2255,
Melbourne, FL 32902-2255.
8. Known bondholders, mortgages, and other security
holders owning or holding 1 percent or more of total
amount of bonds, morfoges or other securities: none.
9, Extend and Nature of Circulation:
Average Single
12 Mos. Issue
850 850
A. Total No. copies Printed (Net Press)
B. Paid Circulation
1. Soles through dealers and carriers,
street vendors and counter sales
2. Moil subscriptions
C. Total Paid Circulation
D. Free Distribution (including samples)
by moil corner or other means
E. Total Distribution (Sum of C&D)
F. Office use, left-over, unaccounted
and back start subscription copies
G. Total (Sum of ESF)-should equal net
press run shown in A.
I certify that the statements mode by me above are correct and
complete.
(signed) R. Tucker Abbott, Editor
none
none
735
730
735
730
18
18
753
748
91
102
850
850
THE BEST OF THE
An Exciting and Nostalgic Glimpse
Into Conchologys ftist
Heii' IS a IreiTSLirv of iinsl.Tlf^n and ofton
humorous writings takfii from tho first 40
voars of America's oldest mollusk |ourn,il,
covering the Lite pioneering f^'riod of
1886 to 1927 The noted m.iKicoiogist and
editor, R Tucker Abholl has carefully
gathered a wide-ranging series of over
100 articles that depict tiir lore and ex-
citement of sli.'il hunlmt; in the United
States
American M«lacologlst5
P.O. Bo. 2255 288 pp , rinthbound $13,95.
Melbourne, FL 32902-2255
Collectible Shells
of Southeastern U.S., Bahamas
& Caribbean by R, Tucker Abbott. Ph d
A 'Take it to ttie Beach' Field Guide
WATERPROOF - TEARPROOF
105 beautiful color photos of living animals and
their shells 64 pages ol color 300 species il-
lustrated. How to clean shells. Where to find
them. Includes fossils, pond and tree snails, as
well as sealife
Collectible Shells stresses conservation, but
also has helpful hints about collecting and
cleaning shells. The book introduces the tourist
and beginner to famous Florida fossils and the
unique world ol tree and pond mollusks
Printed on a washable, tearproof plastic paper.
Drop it in the ocean, use it in the ram, or let your
wet shells drip all over it. Keep it on your boat or
take It to the shore A popular new seller retailing
(or $8.95 Postage a id state lax are included as a
big savings
American Malacologists, Inc.
Publishers of Distinctive Books on Mollusks
P.O. Box 2255, Melbourne, FL 32902-2255
W« accept VISA Of MASTERCARD orders Dymai' Piea";e give dale o' e«
pifation »n(j youf ctfd number Fo'eigr* customers may send mte'na
lionai postal money order ot checK on New Yofh bank o' U S cash by
'egisiered mail
Vol. 100(1) January .31, 1986 THE NAUTILUS
The Nautilus
ITS 100th ANNIVERSARY
and
Volume 100
Dedicated to all the mollusk enthusiasts, both private concholog-ists and pro-
fessional malacologists, who founded and carried on for the last one hundred
years America's oldest journal devoted exclusively to the study of mollusks. To
its 500 contributors and 15 consulting editors are added many thanks and
appreciation.
DEDICATED TO THE FORMER EDITORS^
William D. Averell (1853-1928)
Founder of the Conchologists' Exchange, 1886
Henry A. Pilsbry (1862-1957)
Founder, editor of The Nautilus, 1888-1957
Charles W. Johnson (1863-1932)
Business manager, 1890-1932
Horace Burrington Baker (1889-1971)
Business manager, co-editor 1932-1957
Editor, 1958-1970
Charles B. Wurtz (1916-1982)
Co-editor, 1958-1974;
consulting editor, 1974-1982
Bernadine B. Baker (1906-living)
Business manager, 1958-1979
Morris K. Jacobson (1906-1980)
Consulting editor, 1972-1980
William J. Clench (1897-1984)
Consulting editor, 1972-1984
Joseph Rosewater (1928-1985)
Consulting editor, 1972-1985
'The present staff is R. Tucker Abbott, co-editor, 1958-1969,
editor since 1970; Cecelia W. Abbott, business manager,
since 1979; M. G. (Jerry) Harasewych, associate editor,
beginning with this volume. Mrs. H. B. Baker, former
business manager, lives in Haverford, Pennsylvania.
2 THE NAUTILUS January 31, 198f;
BIRTH AND GROWTH OF THE NAUTILUS
Vol. 100(1)
It was the year 1886. The country was recov-
ering from the depression of 1884. President
Grover Cleveland, in his first term, was about to
dedicate the newly erected Statute of Liberty in
New York harbor. There were still 12 states to
be added to the Union, and it took a two-cent,
brown postage stamp with Washington's like-
ness to send a letter across the country. In
Philadelphia the only means of transportation
were horses, bicycles, the steam locomotive and
boats on the Delaware River. The Academy of
Natural Sciences of Philadelphia had not built
its large new annex and still used gas lights in
its halls and study rooms. In England, they were
celebrating Queen Victoria's Diamond Jubilee,
and the Spanish American War was still 12
years away.
In 1886, in some respects, it was the best of
times for American conchology. William H. Dall
of the U.S. Geological Survey in Washington,
D.C. had already produced over 50 major works
on mollusks, and Harvard University had just
published the first part of his famous "Blake
Report" on deepsea mollusks. George W. Tryon,
Jr., the Philadelphia author of "Structural and
Systematic Conchology," had just completed the
tenth volume of his monumental "Manual of
Conchology." Verrill and Bush in New England
were at the height of their reports on the dredg-
ings of the Steamers FUh Hnivk and the
AlbatToss. William G. Binney, living in New
Jersey, just across the river from Philadelphia,
had just revised his classic "Manual of North
American Land Shells." The Conchological Sec-
tion under the wing of Philadelphia's Academy
was nourishing with such active members as S.
M
/ y y ' ^
7 / // y
o-vSr ^-^ ' -'^/^
■J 11 ^Hy//X
Tho end (if a letter written in Dec. 18i»0 to the editors of the newly launc-hiMl XnuiWux hy
the Calil'ornia-liased shell collector and newspaper editor, Kdward Warren Ro(ier, admon-
ishing them to have it "come out on time."
Vol. 100(1) January 31, 1986 THE NAUTILUS 3
$1.00 per Year. ($1.12 to Foreign Countries.) lOcts. a copy.
THE
NAUTILUS
A MONTHLY
DEVOTED TO THE INTERESTS
OF CONCHOLOGISTS.
EDITOR:
H. A. PiLSBRT, Conservator Conchological Section, Academy of Natural Sciences, Philadelphia.
ASSOCIATE EDITOR :
C. W. Johnson, Acting Curator Wagner Institute of Science.
Vol. VI. FEBRUARY, 1893. No. 10.
CONTENTS:
PAGE.
Additional Shells from the Coast of Southern Brazil. Wm. H.
Dall 109
Description OF A NEW FORM OF CYPR.iiA. John Ford 112
Vol. 84 JULY, 1970 No. 1
THF
NAUTILUS
THE PILSBRY QUARTERLY
DEVOTED TO THE INTERESTS OF CONCHOLOGISTS
EDITORS AND PUBLISHERS
R. Tucker Abbott, du Pont Chair of Malacology
Delaware Museum of Natural History. Greenville. Del. 19807
Horace Burrington Baker, 11 Chelten Road, Havertown, I'a.
(Emeritus Professor of Zoology, University of Pennsylvania)
Charles B. Wurtz, Biology Department
La Salle College, Philadelphia, Pa. 19141
CONTENTS
The occurence of Cymatiidae and Cypraeidae in
North Carolina. By Hugh J. Porter 1
Eggs and attachment sites for egg capsules of Valvata lewisi.
By B. Z. Lang and N. O. Dronen, Jr 9
THE NAUTILUS
January 81, 1986
Vol. 100(1)
Vol. I. No. 1.
This is the first issue of "The Conchologist's
Exchange " As encouragpnient is received it will
assume the form of a printed sheet with columns for
" Exch.-inges in Mollusca," "New Localities," "Answers
to Correspondents," ike. This, our first number, has
been sent to 500 Conchologists. Subscription price, 25
cents per annum, post paid. Exchanges of 20 words, 10
cents; for each additional 10 words the charge will be 5
cents. The Conchologist's Exchange will be issued
semi-monthly, and will endeavour to become a cheap
and useful medium for the exchange of those most beauti-
itful productions of nature — "The Mollusks."
EXCHANGES FOR MOLLUSCA ONLY.
CVPR.^A erosa, L. lynx, L.
CERITHIUM. maculosum,
Kien. eburncum Brug.
CVCLOS rOMA sulcatum. Lam.
clegans Mull,
LVMN.-EA lebraTryon
bTROMBINA ^icanahfcra Sby.
Fi-^urclla volcano. Rve. Col-
umbella fulgunns Lam.
Prof. D. S. SHELDON.
Davenport, fa
SUCCINEApuiris L.
HLLIX arbuslorum L.
" ncmomlii L
" ericelorum. Mull.
Toiundato, MuU.
" Upicida L ccllaria Mull
Pupa muscorum, L.
Cionella subcylindriea
E LtHNERT,
Washington, D C.
CONIOBASIS simplex, Suy.
cariiiifcra. Lam. bella, Con.
p«rangulata. Con,
sordiJa L«a symiTielrica, Hald
;bcnum. Lea
MeUntbo subsolida Anth.
Unioriibigjnosus Lea
pustulosus Lea. gracilis, Barnes
w. a; marsh.
Aledo. Illinois
HELIX albolabris. Say. alter-
nata. Say. clauaa.Say.
elevata, bay. fallax, Say.
hirsuta, Say. inflecta, Say.
solilaria, Say. monodon,
Rackett. Sayii. Binncy.
Pupa armifera. Say, corlicana.
Say. Fallax, Say Unio cicgans
Lea, lachrymosus. Lea, parvus,
Barnes
EDWARD A. ENOS,
Connersvillc, Indiana.
NASSAfossataGld.
Purpura saxicola Val.
Amycla gausapata Gas.
Adula falcata Gld.
Acmaea spectrum Esch
scabra. Nuti, pelta, Esch.
Hipponyx cranioidcs. Carp.
G. W. PUIFRBAL'GH,
Greenfield, Indiana.
American and Foreign
Unionidac for exchange.
Send for list.
No responsibility will be ai-
umed for the siaQ(Jing of the
bovc parties.
Address, WILLIAM 0. AVERELL, Proprietor,
CHESTNUT HILL, PHILADELPHIA.
f ^e Conr^ologists' ^H^ange.
A Monthly Publloatlon desltrned for Ood .holOitlerta and Sclentlsta
arenerally. "Wm, D Averell. Editor and Publlaher.
Vol. II-
MARCH and APRIL, 1888.
No. 9.
oojsra?E2sra?s.
Ill,, Wm A.
H, Wnght,
Tbc .Sl.ell-Hcwing MuUuscb of Kliode Island, II, K, C»ipenier,
brief Noics on the LAod and Frcsh-Wner Shells of Mercer Co.
Note* on the Umonidaeof Florida, Dr, S. H. Wnght and Berlii
Lyogyrus. Gill, and oiher American shells, H. A Pibbry,
MarganuiJA Hildrcthiaaa. Lea. U. Shimek, ...
Notes on .^mencao Shells, Rev. Wm. M. Beauchamp,
A Noted Scienust Dead (Geo, W. Tryon, Jr ) From Phila. Public Ledger,
Bell Taps.
Editorial Note*, ,,.....
The CoDchologiSt in Bermuda, J, Matthew JoDe«.
A Collecung Trip to On»et Bay, Maw,. F. C. Baker, .
Exchangei, ......
Suodard Work* oa Conchology
109
110
"5
116
"7
118
119
119
120
CHESTNUT HILL, Philadelphia, I'a.
Slnylo copies, C cents; 50 oenia a year In the United States
and Canada; Foreign Countries, 62 cents; Countrtee not In
Universal Postal Union, 7B cents.
Vol. lUU(l)
January 31, 1986
THE NAUTILUS
Raymond Roberts (Cypraeidae), John Ford
(Olividae), Dr. Benjamin Sharp (Scaphopoda)
and Angelo Heilprin (Florida fossils).
But in the late 1880's, in other respects, it was
the worst of times for American conchology. It
was like the changing of the guard. Aging Isaac
Lea died in 1886 at the age of 95; Lucy Say,
widow of America's first conchologist, died on
Nov. 15, 1887, and Andrew Garrett, the con-
chologist of the South Seas, died the same
month. Then, like a clap of thunder, George
Tryon, at the age of 49, succumbed to a heart
attack on February 5, 1888, soon after a walk in
a severe winter storm. It was a time when there
was no journal in America devoted solely to mol-
lusks. Tryons American Journal of Conchology
had succumbed in the financial panic of 1873.
In Europe, in 1886, there were eight respecta-
ble scientific journals devoted solely to mollusks
-two each in England, Germany and France
and one each in Belgium and Italy (Jutting and
Altena, 1958). For their outlets, American
malacologists depended on the general publica-
tions of the Smithsonian Institution, the Califor-
nia Academy of Sciences, Harvard's Museum of
Comparative Zoology, and the Academy of
Natural Sciences of Philadelphia.
The need for a new American serial publica-
tion was evident. There were several hundred
active conchologists in United States and
Canada, many of them already publishing
privately or in obscure natural history
magazines. Among them were Henry Hemphill,
Temple Prime, R. E. C. Stearns, T.H. Aldrich,
W. W. Calkins, Charles T. Simpson and Victor
Sterki, to mention but a few.
The Nautilus had a very inauspicious begin-
ning. William D. Averell, a 33-year-old shell
dealer and close friend of Tryon's living in near-
by Chestnut Hill, began the predecessor of The
NautiliLs as the Conchologists' Exchange in July
1886. Volume 1, number 1 was merely a post-
card sent out to 500 people announcing that the
annual subscription price for this monthly
4-page publication would be all of 25 cents. It
was to contain conchological news, exchange
notices and answers to correspondents. By
February 1887, it had grown to 8 pages and the
price rose to 35 cents. The final number, vol. 2,
no. 9, issued in April 1888, two months after
Tryon's death, had 16 pages. Already it had
served as a publication medium for such well-
known mollusk workers as F. C. Baker, Josiah
Keep of California, C. F. Ancey of Algiers, W.
H. Dall, T. D. A. Cockerell and a Harry A.
Pilsbry (later to call himself, Henry).
But a quirk of circumstances in Philadelphia
changed the history of this journal. William B.
Marshall, a Jessup Student at the Academy and
the assistant to Tryon, left in 1887 to be the
Assistant Zoologist at the New York State
Museum in Albany, and later to serve under Dall
and Bartsch in Washington for 40 years. Just at
this time a young newspaper reporter by the
name of Pilsbry from Davenport, Iowa, and a
contributor to the Conchologists' Exchange,
visited the Academy on his way to seek new
employment in New York. Tryon was favorably
impressed with the 24-year-old amateur con-
chologist who already had considerable know-
ledge about mollusks, was an excellent drafts-
man and had a natural bent for research and
publishing. Upon Marshall's sudden departure
for Albany, Tryon immediately invited Pilsbry
to return from New York and be his new assis-
tant. Pilsbry arrived in November 1887, and
Tryon died three months later.
Pilsbry was elected as conservator of the Con-
chological Section in 1888, and he immediately
plunged into the task of finishing the marine
series of the Manual of Conchology. a publication
that supplied much of his salary. There was a
reawakening of interest in the Conchologists'
Exchange, and in early 1889 a "Prospectus" was
sent out announcing its continuation as The
Na^dihis with Pilsbry as editor and Averell as
business manager. Volume 3, no. 1 began on
May 5, 1889.
According to Pilsbry's colleagues (H. B.
Baker, 1958) the one year's association with
Averell "was none too happy" and, at the end of
volume 4, no. 1, Averell's share was bought out
by another Philadelphian, at the Wagner Free
Institute of Science: Charles W. Johnson. This
ideal partnership lasted for the next 42 years
until Johnson's death in Boston in 1932.
Johnson was a very affable and knowledgable
gentleman whose forte was entomology and
paleontology, as well as malacology. He was
particularly successful in inspiring young
naturalists, and when he moved to Boston in
1903 to assume the curatorship of the Boston
THE NAUTILUS
January 31, 1986
Vol. lOU(l)
Society of Natural History, William J. Clench as
a youngster fell under his spell. Years later,
from 1926 to 1932, Clench was the Curator of
Mollusks at nearby Harvard, and often assisted
Johnson in the business affairs of The Nautilus.
It was Johnson's understanding that Clench
would succeed him as business manager, but
upon the former's death in 1932, Pilsbry (then
69) thought that both editors of The Nautilus
should be in the same city; so H. Burrington
Balcer, one of America's leading land snail ex-
perts and Professor of Zoology at the University
of Pennsylvania, began his association as junior
editor and business manager in October 1932
with volume 46. Meanwhile, Clench in 1941
launched the marine journal, Johnsonia, naming
it after his old mentor.
The Nautilus continued to flourish and grow.
Its history is well-told in the Pilsbry memorial
number of The Nautilus by Dr. Baker (1958, vol.
71, no. 3, pp. 112-115). Pilsbry died on October
26, 1957 at the age of 94, and the editorship of
the journal continued under Baker's capable
hands until his death on March 11, 1971, at the
age of 82.
In April 1958, two junior editors joined The
Nautilus, one being the land snail expert and
aquatic biologist, Charles B. Wurtz (1916-1982)
who had received his Ph.D. under Dr. Baker at
the University of Pennsylvania. At the age of 34
I had left the Smithsonian Institution in 1954 to
become the first occupant of the newly-formed
Pilsbry Chair of Malacology at the Academy. I
became the other junior editor and often
assisted Pilsbry in the preparation of the jour-
nal, sometimes entirely assembling and editing
it during Pilsbry 's winter sojourns in Lantana,
Florida. Also, at this time. Dr. Baker's wife,
Bernadine Barker Baker, known to her family
and friends as "Bunny," took over the business
and subscription management, and continued in
that capacity with great success for the next
twenty years.
In 1969 I helped found and organize the
Delaware Museum of Natural History in Green-
ville, and became the curator of their Depart-
fi^osfEcyds,-
"We propose lo Issue a sjxieen paQ,e iliustraied
acTavQ monrnly journal ol Concholosy to be trailed
THE NAUTILUS.
It will lake ihe place cf ihe Concholoaist's Ex-
change formerly published oy Wm. D Averell, and
will be the successor of that paper. Subscribers lo the
Exchange will be crediied on the books ol the Nautilus
wlih such amounts as may be due thern upon their
subGCrlptlons.
The Nautilus will be under the editorial man-
agement of Mr. Henry A. Pilsbry, Conservator of the
Conchologlcal Section at the Academy ot Natural Sci-
ences, and the successor ot the late Mr. Tryon in the
publication of The Manual of Conchology.
The new Journal is designed to afford a medium
of communication between siudents and others interesi-
ed in conchology [ to publish original articles contrib-
uted by amencan and foreign authors^ to record new
discoveries) and lo teach beglnnerG and young studenis
of science.
America needs a Journal ol this kind, and if we
can obtain sufficient encouragement In the shape ol
subscriptions we will commenca the publication of The
Nautilus at once. We enclose yju a blank for your
subscription. If you think well of the prjject please
fill it up at once and return it to
Mouni Airy, PriUadalphic. Pi
The Nautilus.
JANUARY, 1896.
TO C0NCH0L0QIST8.
We regret the necessity which compels ua to start the new year
with an editorial of this nature; but it is nothing new to hear that
the Nautilus must struggle for existence. This struggle has con-
tinued since the Jura, until now we have but a few species, three or
four in the Indo-Pacific and one in the United States. Do vou in-
tend that the only recent Nautill's In North America shall be-
come extinct ? We are willing lo supply the care, but not the en-
tire environment. It needs feeding once a nionth in order to add
another septum. You are asked to assist in this important function
once a year ; and when you see a slip of paper which reads, " Inclosed
please find $1,00," it mean.s that it hasconie your turn to " chip in."
We hope that you will no longer neglect these little reminders.
They mean that your subscription is due. We cannot wait until the
end of the year— U'<; mt(a( have \i in advance.
Wishing you all a Happy New Year.
H. A. P. A C. W. J.
Vol. 100(1)
January 31, 1986
THE NAUTILUS
ment of Mollusks. I moved The Ndutilns. now
owned by Mrs. Baker, to Delaware. In 1979,
upon the recommendation of Bunny, my wife,
Cecelia White Abbott, took over the duties of
business manager.
There was need for an improvement in the
format of the journal which had remained un-
changed for several decades. In May 1972
(volume 86) the page size was increased to 8 x
IOV2 inches, a two-column format established on
a glossy paper, and a board of 13 consulting
editors formed. By now, 85 years after its incep-
tion, the annual subscription rate had risen from
25 cents to $7.00 for individuals. Today it stands
at $15.00.
With the demise of the Department of
Mollusks at the Delaware Museum in 1979 as a
functioning, scientific entity, we moved The
Nautilus, now under the jurisdiction of my
American Malacologists, Inc., to Melbourne,
Florida, where it has been published for the last
six years. We have now added an associate
editor, Dr. M. G. (Jerry) Harasewych, a newly
appointed associate curator in mollusks at the
U.S. National Museum in Washington, D.C.
For over twenty years The Nautilus served as
the official organ of the American Malacological
Union at no cost to their organization. Proceed-
ings of the meetings were published by them
from 1932 to 1953 in the same format as that of
The Nautilus. Like all growing organizations,
the AMU eventually required its own periodical
and now issues the extensive American Mala-
cological Bulletin {vo\. 1, no. 1, July 1983) under
the capable editorship of Dr. Robert S. Prezant
of the University of Southern Mississippi.
The life of an editor is not easy, especially in
the case of scientific journals that constantly
need financial help. The editors of the privately
owned Nautilus were no exception, and they
had to make repeated appeals for subscribers to
"pay up." (Pilsbry and Johnson, 1893). In my 28
years of experience as an editor I had to face
financial and production jiroblems, and I some-
times found manuscripts poorly written, badly
organized, without nomenclatorial knowledge
and often lacking references to the very same
subject. It is work getting some of them into
shape, and sometimes there is little thanks.
There is an old adage that "the next time you see
an understanding and beloved editor, you will
see him laid out horizonally and surrounded by
flowers."
But there are rewards -a sense of accomplish-
ment and the joy of creating- a sense of helping
others to participate in "our glorious science of
conchology" as Averell put it so often in his
editorials of a hundred years ago. A few years
ago I gathered together and published a collec-
tion of interesting articles and reproductions of
ancient advertisements (Abbott, 1975). In The
Best of The Nautilus one can sense the spirit of
comradship among our early contributors. The
Nautilus is for both the lieginning scientist, the
enthusiastic amateur with new discoveries, as
well as for the accomplished malacologist on the
"cutting edge of the science" and immersed in
"the state of the art." It is still a joint and
cooperative effort. Let's hope that The Nautilus
goes on for another 100 years!
-R. Tucker Abbott, Melbourne, Florida
LITERATURE CITED
Abbott, R. Tucker. 1958. From the Pilsbry Chair of
Malacology. The Nautilus 71(3):100-103.
(editor). 1975. The Best ofTheNnutilus. 280 pp.,
American Malacologists, Inc., Greenville, Delaware.
1979. Bernadine Barker Baker -A Tribute upon
her Retirement. The Nnutiliis 93(2-3):ii.
1983. Charles B. Wurtz-An Obituary. The
Nautilus 97(1 ):43. portrait.
f331 RENEWAL OF SUBSCRIPTION
Enclosed find Two Dollars for one year's subscription to THE NAUTILUS,
234 Berkeley Street, Boston, Mass.
Name,
Address,
Notice.— The rules now governing second-class matter do not permit publications to be mailed to
subscribers in arrears.
8 THE NAUTILUS
January 31, 1986
\'(il. 10(1(1)
Abbott, R. Tuckor ami Chas. B. Wurtz. 1971. Horace
Burrington Baker, 1889-1971. (An ol)ituary). The Nautilus
85(l):l-4. 3 portraits.
Avereli, William D. (1899). Pospectus for Tlie Nautilus.
1 page, privately printed. Mt. Airy, Philadelphia, Penna.
Baker, H. Burringti)n. 1958. Henry Augustus Pilsbry,
1862-1957-An Obituary. The Nautilu.'< 71(3):73-83,
3 portraits.
1958a. The Pilsbry Nautilus. The Nautilu.s
71(30):112-115.
Gray, Arthur F. 1933. Charles WillLson Johnson, 18()3-1932.
(An obituary). The Nautilus 46(4): 129- 136, portrait.
.Jutting, W. S. S. Van B. and C. 0. van Regteren Altena.
1958. A list of Printed Malacological Journals. Basteria
22:10-15, 1 graph.
Pilsbry, H. A. and C. W. Johnson. 1893. To Conchologists
(a piea for support). The Nautilus 7(3):25-26.
Wurtz, Charles B. 1958. Dr. Pilsbry and Fresh-water
Mollusca. The Nautilus 71(3):84-87.
TOM PULLEY AND THE TRAIN
Thomas Edward Pulley, born October 15, 1916, Director of the Houston
Museum of Natural Sciences since 1957, and a malacological student of the late
William J. Clench of Harvard, passed away on Nove^riber 19, 1985, at the age of
69. In preparation for the 100th anniversary volume of The Nautilus, which in
part is dedicated to Dr. Clench, I asked Tom to write a personal anecdote that
typified his mentor. If my readers will recall, in my "Farewell to Bill Clench"
(The Nautilus 9S(2):55-58), Bill drew a huge arrow in the sandy beach for his
students that pointed to a waiting train. Tom Pulley has now caught up with the
other students, and here is Tom's personal account of The Train written in July
198U. He asked that this last picture of Bill Clench be included- (RT A).
Everyone who knew Bill was aware of his
capacity for enthusiasm over a new shell. We
who worked with him at the MCZ often wit-
nessed the thrill of anticipation with which he
opened each new package of shells and spread
out the contents on the wide brown table. It was
almost like watching the bright-eyed wonder of
a small child at his first real Christmas.
But Bill had the same happy way of appreciat-
ing most of the other simple pleasures of life. He
and Julia once invited me and my wife and
5-year-old son to a Sunday afternoon picnic; Bill
would grill the hamburgers.
When we arrived at his chosen site I was a bit
surprised to see that we were on a nice grassy
spot, but it was on the railroad-right-of-way.
There were houses nearby, but they were mostly
concealed by trees. I had known that Bill liked
trains, and I soon learned that we were here to
wave at the afternoon train when it passed by.
We lighted the charcoal and opened some beer
and cokes.
When the coals were ready. Bill grilled the
hamburgers and they were delicious. As we
were finishing I saw that Bill key)t glancing at
his watch. Soon we heard the faint whistle of
William J. Clench, age 8G, in California.
Vol. 100(1)
JanuarvSl, 1986
THE NAUTILUS 9
one of the last steam trains, and Bill quickly
jumped to his feet. He strained to view the big
engine when it first came into sight around a
distant bend, and long before it was near us he
raised both hands in the air and began to wave.
As the train approached he began jumping in
the air and waving more excitedly. The engineer
saw him and began tooting his whistle in a long
series of short bursts. The excitement was
catching, and by the time the engine had
reached us my son was as excited as Bill, and I
was amazed to find that I, too, was jumping and
waving like a 5-year old. The smiles that were
exchanged between Bill and the engineer as the
train roared by led me to believe that this must
have happened many times before.
I understood Bill's joy that afternoon as the
train passed by, because I had taken part in it. I
later realized that Bill experienced this same
kind of happy pleasure in many of the less
dramatic events of daily life. To Bill, the thrill of
seeing a new shell, meeting an old friend or
making a new one, finishing another number of
Johnsonia, or even telling one of his old bad
jokes was comparable to his pleasure that day by
the railroad tracks. - Tom Pulley, Julv 1984
JOSEPH ROSEWATER (1928-1985)
A TRIBUTE AND BIBLIOGRAPHY
Harald A. Rehder
Smithsonian Institution
Washington, D.C. 20560
On March 20, 1985, malacologists the world
over lost an eminent and treasured colleague,
and those close to him a dear friend. His un-
timely death left a void in the ranks of malacolo-
gists that will be hard to fill, and his associates
at the Smithsonian still find it difficult to believe
that we will not see him at any moment leaving
his room or coming around the corner in the
halls or in the range of the Division of Mollusks.
Joe was born on September 18, 1928 in Clare-
mont. New Hampshire, in the Connecticut River
Valley, the only child of Joseph and Alice
Tipping Rosewater. His mother had come to
Claremont from the Rosewater home in Queens,
Long Island, New York, to be with her parents
at this time.
Joe's father was an accountant with the City
of New York, and his mother had been a Navy
nurse in World War I. When Joe was eight years
old his father died. Joe graduated in June 1946
from John Adams High School in South Ozone
Park, Long Island, two months after the death
of his mother. Joe's mother, before her death,
had appointed her brother Charles to be Joe's
legal guardian, and therefore Joe moved to his
uncle's home in Claremont, New Hampshire.
In the fall of 1946 Joe entered the University
of New Hampshire at Durham, graduating in
1950. As a boy he had had an interest in animals,
and had kept an aquarium in his room. His
special interest in mollusks began apparently in
FIG. 1. .Jo.suph RusuwaliT ui a I'ui-fiit iiitVirnial puse.
10 THE NAUTILUS
January 31, 1986
Vol. 100(1)
his junior year at the University when his
zoology professors, Emery F. Swan and George
M. Moore, persuaded him to undertake a mollus-
can project for a master's degree. This is
evidenced by the fact that Joe states that his
first field work started in 1949 with collecting
mollusks in New England.
Joe began working on his Master's degree in
the fall of 1950 but his plans were interrupted by
the arrival of a draft notice in February 1951.
That month he married Mary Carlson of Gilman-
ton, New Hampshire, and in May he was formal-
ly drafted and went to Fort Meade, Maryland,
for basic training. In the fall he was sent to Fort
Sam Houston, Texas, to receive further training
as a medical technician in radiology. In early
March 1952 Joe was sent overseas to Germany
where until April 1953 he was a medical techni-
cian in radiology in the 97th General Hospital in
Frankfurt-am-Main.
After his return from Germany and after leav-
ing the service, Joe worked as an x-ray tech-
nician at the Sacred Heart Hospital in
Manchester, New Hampshire, and as an instruc-
tor in biology at Mount St. Mary's College in
nearby Hooksett until May 1955. That summer
he enrolled at the University of New Hamp-
shire, attending the summer school and then the
academic year 1955-56, receiving a Master's
degree in June 1956.
In the fall of 1956 he entered Harvard Univer-
sity as a graduate student to work under Dr.
William J. Clench in malacology. Here, in the
company of Richard I. Johnson, Richard W.
Foster, Robert Robertson, Arthur H. Clarke
and Arthur S. Merrill, he spent four happy and
fruitful years under the genial and caring
tutelage of Bill Clench and Ruth Turner.
In the summer of 1957 Joe came to Washing-
ton and spent three months in the Division of
Mollusks of the U. S. National Museum as a
Summer Intern, working on the family Pleuro-
ceridae in connection with his doctoral studies.
In the course of his studies he reorganized the
North American members of the family
Thiaridae in the museum collection.
The following summer Joe accompanied Bill
Clench on a field trip through Kentucky, Ten-
nessee and Georgia, collecting and studying the
freshwater faunas of the area.
During his years at Harvard Joe was a Teach-
ing Fellow in Biology, and in his last year he
held a position as Curatorial Assistant in the
Department of Mollusks. In the fall of 1959,
Joe's final year at Harvard, Bill Clench and Joe
were beginning to plan for Joe's immediate
future after he received his degree in the coming
June, and Bill wrote to me regarding a possible
opening at the National Museum. For a year or
more we had on file a job application form that
Joe had filled out for a position in the Division,
awaiting the time when we would get approval
to hire an additional staff member. At this time
the opportunity opened up to hire a malacologist
under a grant that the National Museum had
received from the Office of Naval Research and
Atomic Energy Commission (ONR-AEC) to
work on the marine faunas of the Pacific,
especially that of the Marshall Islands- Bikini
and Enewetak.
This position was offered to Joe and he started
working on January 1, 1960. In the year and
nine months that he was on this contract he
helped identify and arrange many lots of Indo-
Pacific mollusks, and spent several days a week
reorganizing and expanding the collections of
Indo-Pacific marine mollusks, bringing the
classification up to date and adding thousands of
lots to the collection. In August 1961 Joe made
his first visit to the Pacific attending the Tenth
Pacific Science Congress in Hawaii.
On October 2, 1961 Joe joined the staff as
Associate Curator, and for the next twenty-
three and a half years was a valued and impor-
tant member of the scientific staff of the
National Museum of Natural History.
With the addition of Joe, the staff of the Divi-
sion of Mollusks was once more at full strength,
and this fact seemed to infuse new energj' into
the divisional activities, stimulated in part no
doubt by Joe's enthusiasm in his new position.
Recorded in the annual report for that year was
a notable increase in the number of specimens
distributed in exchange, lent for study and iden-
tified for correspondents.
Although Joe's doctoral dissertation dealt
with a freshwater mollusk, marine mollusks
were his first love, as he told me in a letter he
wrote when I offered him the opportunity of
coming to the Smithsonian on the ONR-AEC
grant. He had just finished preparing for the
cataloguer the last of the marine collection of
Vol. 100(1)
January 31, 1986
THE NAUTILUS 11
the old Boston Society of Natural History that
had been turned over to the Museum of Com-
parative Zoology', and was in the midst of incor-
porating Tucker Abbott's Philippine marine
shells into the collection. When he came to work
in the Division under the grant, sorting and
classifying the Indo-Pacific moUusks was,
therefore, a familiar task. After he and Ruth
Turner had finished the western Atlantic Pin-
nidae they had planned to monograph the Indo-
Pacific species of the family. Now Ruth sug-
gested that Joe do the paper alone, and this he
did. He finished the project and it was published
before the end of his contract. Following this he
began studying the family Tridacnidae and the
Indo-Pacific Littorinidae, both of which were
eventually published in 1965 and in 1970/72. He
continued his interest in these three families and
published several papers. He was working on a
study of the Eastern Pacific members of the
Littorinidae at the time of his death, and also
had underway a study of the bivalve family,
Periplomatidae.
During his years in the Division of Mollusks
Joe went on several expeditions and field trips.
In February and March 1963 he spent six weeks
at the Enewetak Marine Biological Laboratory
of the Atomic Energy Commission, and that
winter he spent three months in the western
Indian Ocean on the research vessel Te Vega as
part of the International Indian Ocean Expedi-
tion. In August and September 1966 Joe was in
Australia spending most of the time carrying on
field work in Western Australia with Barry C.
Wilson, and in May and June 1970 he was a
member of the Mariel King Memorial Moluccas
Expedition on the R/V Pele. again together with
Barry Wilson. In April 1974 he spent two weeks
in Tunisia at the Mediterranean Marine Sorting
Center, and in July 1976 he was a member of a
party from the Smithsonian that spent ten days
making a survey of the littoral fauna of Ascen-
sion Island. Later he made several trips to
Panama, and to the Pacific coast, including
Alaska, in connection with his study on the Lit-
torinidae of that fauna. His last trips away from
Washington were to the Harbor Branch Labora-
tory at Fort Pierce, Florida where for several
years he carried on field studies on Periploma
and the Littorinidae.
Joe was a member of the American Malacolo-
gical Union from 1957 on and was its President
in 1969. He was also a member and past presi-
dent of the Biological Society of Washington,
the Society of Systematic Zoology of which he
was treasurer 1963-1966, and the Paleontolo-
gical Research Institute, Ithaca, New York. He
was a member of the National Capital Shell Club
and its president in 1965. He served as a Con-
sulting Editor of The Nautilus from 1972 to
1984, and contributed 17 articles to that journal.
In the Museum he represented the Depart-
ment of Invertebrate Zoology on several com-
mittees-the Professional Advancement Evalu-
ation Committee, the Council of the Senate of
Scientists, and the Advisory Committee on the
Naturalist Center. On the Departmental Collec-
tions Advisory Committee he represented the
Division of Mollusks.
Joe is survived by his wife Mary Carlson
Rosewater and three children, Katherine Louise
Rosewater (Waitt) of Sandown, New Hamp-
shire, Gail Ann Rosewater of Rockville, Mary-
land, and Carl Joseph Rosewater of Kensington,
Maryland, and a granddaughter, Megan
Rosewater- Waitt.
Bibliography of
Joseph Rosewater
1957. A comparative study of development in the Peri-
winkles. Abstracts of student research projects. Woods
Hole Embryology Counie. 1957:14-15, 1 table.
1958a. The Family Pinnidae in the Western Atlantic.
Johnsonia 3(38):285-326, 23 plates (with Ruth Turner).
1958b. Book Review: Olsson, A., et al. Pliocene Mollusks of
Southern Florida, etc. Johnsonia 3(38):328.
1959a. Mollusks of the Salt River, Kentucky. The Nautilus
73(2):57-63.
1959b. Intertidal stranding of Clione limacina in Massa-
chusetts. TheNautUux 73{2):76-n.
1959c. Calvin Goodrich, a bibliography and catalogue of his
species. Occasional Papers on MoUusks. Department of
Mollusks. Museum of Comparative Zoology. Hanmrd
University. 2(24): 189-208, 1 photograph, 1 plate.
1959d. A Pleurocerid index to past collecting in the Ohio
and Tennessee River Basins with some thoughts for the
future. Annual Report American Malacological Union
for 1958, Bull. 25:23-24.
1960a. Egg mass and gross embryology' of Pleurocera
canalicutata (Say, 1821). Annual Report .\merican Mala-
cological Union for 19.59, Bull. 26:10-12.
1960b. Proposed further use of the Plenary Powers in the
case of the Generic name Pleurocera Rafinesque, 1818
(Class Gastropoda). Z.M.(S)83. Bulletin of Zoological
NoTnenclature 17(6-8):171-172.
1961a. Preliminary observations on the nervous systems of
12 THE NAUTILUS
January 31, 1986
Vol. 100(1)
some Pleuroceridae. Annunt Report American Mahi-
cological Union for 1961, Bull. 28:10-11.
1961b. Comments on the proposal to place the Generic name
Gari Schumacher, 1817, on the Official List, Unemended,
Z.N.(S)1461. Bulletin of Zoological Nomenclature
18(5):303.
1961c. The Family Pinnidae in the Indo-Pacific. Indo-
Pacific Mollwica l(4):17.'5-226, pis. 135-171, figs., maps.
1963a. Resistance to dessication in dormancy by Tectariux
muricatuit. The Nautilus 76(2):111.
1963b. An effective anesthetic for giant clams and other
mollusks. Turtux News (Chicago) 41(12):300-302, 2 figs.
1963c. Problems of species analogues in world Littorinidae.
Annual Report Anifrican Malacolociical Union for 1963,
Bull. 30:.5-6.
196.5a. The Family Tridacnidae in the Indo Pacific. Indo-
Pncific Mollusra l(6):347-396, pis. 263-293.
19651). Studying living Tridacnidae in the Marshall Islands.
Annual Report American Malacological Union for 1965,
Bull. 32:18-19.
1966a. Reinstatement of Melarhaphe Menke, 1828. The
Nautilus 80(2):37-38.
1966b. The Giant Clams. Australian Natural History 1.5(8):
250-256. 5 figs.
1967a. Indo- West Pacific Littorinidae. Aurnial Report
American Malacological Union for 1966, Bull. 33:27.
1967b. Book Review: Halstead, B. W. 1965. Poisonous and
Venomous Marine Animals of the World, vol. 1, Inverte-
brates. Science 156(3776):795 (with M. L. .Jones, R. B.
Manning, D. L. Pawson, and K. Ruetzler).
1968a. The Zoological Taxa of William Healey Dall. Bulletin
U. S. National Museum 287:1-427 (with K. J. Buss and
F. A. Ruhoff).
1968b. Itinerary of the Voyage of H. M. S. Blossom. The
Veliger 10(4):'350-352.
1968c. Book review: Hyman, L. H. 1967. The Invertebrates,
vol. VI. Mollusca 1. Science 160(3823):62-63.
1968d. Book review: An English-Classical Dictionary for the
use of Taxonomists. Systematic Zoology 17(3):334.
1968e. Notes on Periplomatidae (Pelecypoda: Anomalodes-
mata) with a geographical checklist. Annual Report
American Malacological Union for 1968, Bull. 35:37-39.
1969a. (iross anatomy and classification of the commensal
gastropod, CaledonieUa montrouzieri Souverbie, 1869.
The Veliger ll(4):345-350, text figs. 1-4, pi. 55.
1969b. George Mitchell Moore. 1906-1968. [Obituary]. The
Nautilus 9,ZC[):\\\.
1969c. Comment on a review by ,J. D. Rising of R. E. Black-
welder, Taxonomy, a Text and Reference Book. Systema-
tic Zoology 18(3):361-362.
1969d. Malacological collections-development and manage-
ment. In: Natural History Collections, Past- Present -
Future, Symposium of the Biological Society of Washing-
ton. Proceedings of the Biological Society of Washington
82:663-670.
1970a. The Family Littorinidae in the Indo-Pacific. Part I.
Subfamily Littorininae. Indo-Pacific Mollusca 2(11):
417-506, 64 plates.
1970b. Monoplacophora in the South Atlantic Ocean. Science
167(3924):1485-1486, fig.
1970c. Another record of insect dispersal of an Ancylid
snail. TheNautihis 83(4):144-145.
I97()d. The role of the professional in Malacologj-. Pitts-
hurgh Shell Club Bulletin 5:12-13.
1970e. Book Review of: .Johnstone, Kathleen Yerger. Col-
lecting Seashells. Grosset and Dunlap. Illus., 198 pp.
Atlantic Naturalist 25(4):187-188.
1970f. Discussion of: R. T. Abbott, Eastern Marine Mol-
lusks. In: American Malacological Union Symposium on
Rare and Endangered Mollusks. Malacologia 10(1):49.
1972a. The Family Littorinidae in the Indo-Pacific. Part II.
The Subfamilies Tectariinae and Echinininae. Indo-Pacific
Mollusca 2(12):507-534, 21 plates.
1972b. Book Review: Wilson, Barry R. and Keith Gillett.
1971. Australian Shells. National Capital Shell Club
Newsletter February 1972, 2 pp.
1972c. Book Review: Brost, F. B. and R. D. Coale. 1971.
A guide to Shell Collecting in the Kwajalein .-Xtoll.
National Capital Shell Club Newsletter February 1972,
2 pp.
1972d. The Amphi-Atlantic distribution of Liltorina melea-
gris. The Nautilus 86(2-4):67-69, plate, map. table (with
G. .J. Vermeij).
1972e. Teratological Littorina scahra angulifera. The
Nautilus 86(2-4):70-71, plate.
1972f. Life spans of Mollusca. In: Altman, P. L. and D. S.
Dittmer. 1972. Biology Data Book, edition 2, vol. 1,
pp. 234-235. Federation of American Societies for Experi-
mental Biologj', Bethesda, Maryland.
1973a. Book Review: Wilson, B. R. and Keith Gillett. 1971.
Australian Shells. The Quarterly Rerieiv of Biology
48(l):42-43.
1973b. Book Review: Graham, Alastair. 1971. British Proso-
branch and other Operculate Gastropod Molluscs. The
Quarterly Review of Biology 48(1):43.
1973c. A Source of Authors and Dates for Family Names of
Gastropods. The Veliger 16(2):243.
1973d. Replacement pages for: The Family Littorinidae in
the Indo-Pacific, Part II, the Subfamilies Tectariinae and
Echinininae (Indo-Pacific Mollusca 2(12):509-516).
Indo-Pacific Mollusca 3(14):63-70.
1973e. More on Penis Shedding Among L('/ion)ja. Neir York-
Shell Club Notes, no. 196, November 1973, p. 7.
1974a. Studies on Ascension Island Marine Mollusks. Bulk-
tin American Malacological Union for 1973, pp. 30-32.
1974b. Phylogeny of Littorinidae. Littorinid Tidings.
Occasional Newsletter of Littorinidae Research Grotip,
no. 1, pp. 10-11.
1975a. An Annotated List of the Marine Mollusks of Ascen-
sion Island, South Atlantic Ocean. Smithsonian Contri-
butions to Zoology 189:1-41, figs. 1-24, 3 tables.
1975b. The Marine Commensal Gastropod, CaledonieUa
mxmtrouzieri (Prosobranchia: Hipponicacea) in Thailand.
The Nautilus $%iyM.
1975c. Mollusks of Gatun Locks, Panama Canal. Bulletin
American Malacological Union for 1974, pp. 42-43.
1975d. Book Review: R. Scase and E. Storey. 1975. The
World of Shells. National Capital Shell Chih Neu'sletter.
September, 1975. p. 10.
1976a. William Healey Dall, The Legacy He Left for Mala-
cology. Bulletin American Malacological Union for 1975,
pp. 4-6.
1976b. The NMNH-STRI Survey of Panama 1971-1975.
Bulletin American Malacological Union for 1975,
Vol. 100(1)
January 31, 1986
THE NAUTILUS 13
pp. 48-50.
1976c. Letter U> the Editor. AiistnilniH Slifll ,\eirx No. Hi,
p. 2.
1976(1. Book Review: Ruth Fair. Shell Collectors' Cuide.
National Capital Shtil Cliili Ni-iivlettrr. Septemlier 1976,
pp. 11-12.
1976e. Application to use Plenary Power to designate the
type of Pleurocera. Bulletin of Zmilogiral Nnnirnrlatiirr
33(2):10.->-n3.
1977. Bicentennial Booty. National Capital Shrll CluliNcivs-
letter. February 1971, p. 8.
1978a. Zoogeography of West African Littorinidae. Bulletin
Ameriran Malacological Union for 1977. pp. .31-34.
1978b. A Case of Double Primary Homonymy in East Pacific
Littorinidae. The Nautilus 92(3):123-12.5.
1978c. A Malacological Ecpedition to the Moluccas, National
Geiyraphir Society Research Reports nf 1969 Projects.
pp. .515-523. (With Barry R. Wilson).
1978d. Book Review; Kirtisinghe. P. 1978. Sea Shells of
Sri Lanka. National Capital Shell Club Newsletter.
September 1978, p. 11.
1979a. A Reconnaissance of West American Littorinidae.
Bulletin American Malacological Union for 1978, p, 55.
1977b. Rectifications in the Nomenclature of some Indo-
Pacific Littorinidae. Proceedings Biological Society of
Wa.-ihington 92(4):773-782. (with W. F. Ponder).
1979c. Further Comments on the Proposed Designation of a
Type Species for Pleurocera Rafinesque, 1818. Z.N.(S)83.
Bulletin Zoological Nommclature 36(3):139-146. (with
J. P. E. Morrison, A. H. Clarke, G. M. Davis, and C. B.
Stein).
1980a. Predator Boreholes in Periploma margaritaceuni
with a brief survey of other Periplomatidae (Bivalvia:
Anomalodesmata). The VV/7>r 22(3):248-251.
1980b. A Close look at Littorina Radulae. Bulletin Ameri-
can Malacological Union for 1979, pp. 5-8, 8 figs.
1980c. Subspecies of the Gastropod Littorina .•icahra. The
Nautihis 94(4):158-162, 12 figs,
1980d, Book Review: Melvin, A. G. and Melvin, L. S. 1980.
1000 World Sea Shells, Rare to Common with Values.
National Capital Shell Club Newsletter. September, p. 4.
1981a. The Family Littorinidae in Tropical West Africa.
Atlantule Reports 13:7-48, 6 plates, 2 tables.
1981b. A New Aid to Taxonomic Research on Mollusks.
Bulletin American Malacological Union for 1980, p, 67.
1981c. Changes in Shell Morphology of Post Larval Tri-
dacna gigas Linne (Bivalvia: Heterodonta). Bulletin
American Malacological Union for 1980, pp. 45-48, figs.
1981(1. Malacological .'lourney into Cuba, 1980, The Nautilus
95(4):1.59-162,
1981e. Rectifications in the Nomenclature of some Indo-
Pacific Littorinidae -II. Proceedings Biological Society
of Washington 94(4):1233-1236.
1982a. A new species of Hippopus (Bivalvia: Tridacnidae).
The Nautilus 96(l):3-6, 4 figs.
1982b. A new species of the Genus Echininus (Mollusca:
Littorinidae: Echinininae) with a review of the Subfamily.
Proceedings Biological Society of Washington 95(1):
67-80, 6 figs, table.
1982c. Book Review: R. K. Dell, Sea Shore Life. Natiaual
Capital Shell Newsletter. No. 70, Autumn, p. 15.
1983a. Review of Hawaiian Pinnidae and Revalidation of
Pinna exquisita Dall, Bartsch, and Rehder, 1938 (Bivalvia:
Mytiloida). Pacific Science 36(4):453-45S.
1983b. Review of: .lames Graham Cooper- Pioneer Western
Naturalist, by Eugene Coan. The Nautilus 97(l):44-45.
1983e. Another Bivalve-/l/)/(?-o(^j;(7 Association with Com-
ments on Adaptive Significance of Oddly Shaped Lepto-
nacea. American Malacological BuUetiii 1:90-91.
1984a. A bibliography and list of the taxa of Mollusca
introduced by .Joseph P. E. Morrison (December 17, 1906-
December 2, 1983). The Nautilus 98(l):l-9.
1984b. A new species of Leptonacean Bivalve from off
Northwestern Peru (Heterodonta: Veneroida: Lasaeidae).
The Veliger 27(l):81-89. 6 figs. 1 table.
1984c. Burrowing activities of Periploma margaritaceum
(Lamarck, 1801) (Bivalvia: Anomalodesmata: Periploma-
tidae). American Malacological Bulletin 2:35-40, 1 plate,
1 table.
1984d. Bermuda marine Mollusk type specimens transferred
to the Smithsonian. The Nautilus 98(4):151-153.
1985. Epizoan Communities on Marine Turtles 1. Bivalve
and Gastropod Mollusks. Marine Ecology 6(2):127-140,
4 figs., 1 table (with .1. Frazier et al.).
14 THE NAUTILUS
lanuary 31, 1986
Vol. 100(1)
DESCRIPTION OF THE HABITAT OF THE ENDANGERED MUSSEL
PLETHOBASUS COOPERIANUS
Andrew C. Miller
Barry S. Payne
U.S. Army Engineer Waterways
Experiment Station
P.O. Box 631
Vicksburg, MS 39180
and Terry Siemsen
Navigation Planning Support Center
P.O. Box 59
Louisville, KY 40201
ABSTRACT
A total of 26 species ofunionids, in addition to the Asian Clam. Corbicula, were
collected at a mussel bed on the Ohio River near Ohnsted, Illinois. The bed was
dominated by Corbicula (1475/m^, 128.2 g/m^ of Tissue Dry Mass, TDM) and
Fusconaia ebena (66.0/m^ and 39.7lm^ of TDM) although eight other unionids.
Amblema plicata, Elliptio dilatatus, Leptodea fragilis, Ligumia recta, Mega-
lonaias gigantea, Pleurobema cordatum, Potamilus alatus, and Truncilla donaci-
formis were also judged comynon. In addition, three live specimens of the Fed-
erally endangered Orange-footed Pimpleback Mussel, Plethobasus cooperianus,
were identified. All appeared healthy and were adult-sized, ranging in total shell
length from 68 to 7U mm. While there are no records of recent recruitment for P.
cooperianus, it appears that this mussel bed, which contains a diverse cammunity
of bivalves in addition to a dense population o/' Corbicula, provides good habitat
for this particular species.
Three live specimens of the Endangered
Plethobasus cooperianus (Lea 1834), the Orange-
footed Pimpleback Mussel, were found in
September 1983 during a survey of a gravel bar
in the Ohio River near Olmsted, Illinois. In the
summer of 1982, Williams and Schuster (1982)
collected mussels at this site and found a single
live P. cooperianus. However, other workers
brailed this gravel bar and found no live endan-
gered species (Neff & Pearson 1980, Williams
1969). The purpose of this paper is to document
the existence of this species, and to provide in-
formation on habitat characteristics and com-
munity structure where it was collected.
The historical range of P. cooperianus in-
cluded the Ohio River from western Pennsyl-
vania to southern Indiana; the Wabash River
below Mt. Carmel, Illinois; the Cumberland
River from Cumberland County, Kentucky, to
the vicinity of Nashville, Tennessee; the lower
Clincli River in Anderson County, Tennessee;
and the Tennessee River from near Knoxville,
Tennessee, to Kentucky Lake, Benton County,
Tennessee. It has also been recorded from the
Caney Fork, Holston, and French Rivers in
Tennessee and from the Green and Rough
Rivers in Kentucky. At present, P. cooperianus
is restricted to the Ohio and lower Wabash
Rivers where it is uncommon and to the lower
Tennessee River in Alabama and western
Tennessee where it is also uncommon.
The shell of P. cooperianus is up to 87 mm
long, 75 mm high, and 45 mm wide; it is heavy,
subcircular, and tuberculate. The periostracum
is chestnut colored and the nacre is either white
or faintly pink and iridescent posteriorly.
Superficially this species resembles Q.
pustulosa, but the latter species is usually
smaller and has fewer and relatively larger
tubercles which tend to be laterally rather than
radially extended. In addition, Q. pustulosa
exhibits white nacre and young specimens have
prominent green rays, whereas in P. cooperia-
nus the rays are obscure and narrow. The most
definitive characteristic in P. cooperianus is the
bright orange viscera, which can be seen in live
specimens by gently prying the valves apart
(Clarke and Fuller 1983).
Wilson and Clark (1914) reported collecting
two gravid females in June from the Cumber-
Vol. 100(1)
January 31, 1986
THE NAUTILUS 15
land River; evidently it is a summer breeder
although the host fish is unknown. Although
ecological data are virtually non-existent, this is
a large river species which has been collected
from sand and gravel substrate in shoals and
riffles.
Methods and Study Area
On 26-29 September 1983 molluscs were col-
lected from a reach of the Ohio River below
Lock and Dam 53 near Olmsted, Illinois. The
study area included the upper portion of a
mussel bed delimited by Williams (1969) and
Williams and Schuster (1982). During the four-
day study bivalves were collected by hand along
the shore, with the use of a 5-ft brail bar, and by
an experienced shell diver using underwater
breathing apparatus. As part of this work the
diver completed three 30-min qualitative
searches, and collected six 0.25- m^ quadrat
samples from each of four sites on the mussel
bed. This project was undertaken for the U. S.
Army Engineer District, Louisville, to provide
information for a Feasibility Report and Envi-
ronmental Impact Statement for the Lower
Ohio River Navigation Project.
The gravel bar where mussels were collected
was about 3 miles long and followed the Illinois
shoreline. Substrate consisted of densely packed
coarse sand and gravel. Particle sizes varied
from less than 1.0 cm to more than 10.0 cm with
the greatest fraction of total weight in the 1- to
3- cm range. Water depths where P. cooperia-
nus were taken ranged from approximately 3 to
6 m deep. The study site was Ohio River Mile
966.6 to 967.2, approximately 4 miles downriver
of Lock and Dam 53; navigation and barge fleet-
ing were taking place in the immediate area. No
recent evidence of sedimentation, physical abra-
sion, or propeller wash from navigation activi-
ties, were noted at this portion of the gravel bar.
Results
Using qualitative and quantitative techniques,
26 species of unionids, in addition to the Asian
Clam, Corhicula, were collected at or adjacent
to the gravel bar (Table 1). Although nine
species were judged common, the most abun-
dant bivalves were Corhicula, Amblema plicata,
Fusconaia ebena, Lampsilis teres. Megalonaias
gigantea, and Potomilus alatios.
TABLE 1. Bivalves ccillected at a gravel bar near Olmsted,
Illinois. 26-29 September 1983. All taxa were collected alive.
Scientific Name
Family Unionidae
Actlnonaias carinata
Amblema plicata
Cyclonaias tuberculata
Ellipsaria llneolata
Elliptio crassidens
Elliptio diiatatus
Fusconaia ebena
Lampsilis ovata
Lampsilis teres
Lasmigona complanata
Leptodea f ragilis
Ligumia recta
Megalonaias gigantea
Obliquaria ref lexa
Qbovaria olivaria
Flethobasus cooperianus
Plethobasus cyphyus
Pleurobema cordatum
Potamilis alatus
Quadrula metanevra
Quadrula nodulata
Quadrula pustulosa
Quadrula quadrula
TritoRonia verrucosa
Truncilla donacif ormis
Truncilla truncata
Family Corbiculidae
Corbicula manilensis
Presence*
UC
C
nc
FC
FC
UC
c
UC
c
UC
c
c
c
FC
UC
UC
UC
c
c
FC
FC
FC
FC
UC
C
DC
* Presence, for this study:
UC = Uncommon, < 6 collected
FC = Fairly common, 6-20 collected
C = Common, > 20 collected
A total of 14 species of unionids were collected
in 24 0.25-m^ quadrat samples (Table 2). Total
unionid density ranged from 28 to 124/m^ (X =
60). Numerically, F. ebena (X = 46/m^) and Trun-
cilla donaciformis (X=12/m^) dominated the
unionids. Two species, Q. metanevra and Q.
nodulata, judged fairly common in the study
area, were found in only 1 of the 24 quantitative
samples. The gravel bar was numerically domi-
nated by Corbicula, with numbers ranging from
556 to 2628/m' (X=1475). Average tissue dry
mass (TDM) for Corbicula (128.2 g/m') was ap-
proximately three times that for total unionids
(X = 39.7). Because of their large size and high
16 THE NAUTILUS
January 31, 1986
Vol. 100(1)
TABLE 2. Bivalves collected in 24 0.25-ni' quadrat samples at a gravel bar near Olmsted,
Illinois, 28-29 September 1983.
Species
Occurrence*
24
No/m^
1475
TDM/m^
Corbiaula manilensis
128.2
Total unlonlds
Ih
66.0
39.7
Fusconaia ebena
24
45.5
27.4
Truncilla donaaiformis
24
11.5
0.4
Leptodea fvagilis
11
2.5
1.3
Obliquaria reflexa
9
1.8
0.8
Quadrula pustulosa
8
1.5
1.4
Amblema plioata
6
1.0
3.1
Ellipsaria lineolata
7
1.3
1.5
Tritogonia verrucosa
3
0.5
0.4
Lcmpsilis ventrioosa
6
1.2
0.03
Quadrula quadrula
5
0.8
1.3
Quadrula metanevra
1
0.2
0.1
Quadrula nodulata
1
0.2
0.1
Megalonaias gigantea
2
0.3
1.3
Aatinonais aarinata
1
0.2
0.3
* Occurrence - Number of quadrats with live organisms (total quadrats
collected = 24) .
numbers, F. ebena represented the majority,
about 70% (27.4 g/m^ of the total unionid
biomass. Although numerically dominant, T.
donaciformis. because of_ its small size,
represented only about 1% (X = 0.4 g/m^) of the
unionid biomass. Based upon these quantitative
collections, evidence of recent recruitment
(presence of clams less than 12 months old judg-
ing from their small size and unweathered ap-
pearance) was observed for 12 of the 14 unionids
collected in the quadrats.
The three specimens of P. cooperianns were
obtained near Ohio River Mile 967.2 by the diver
during two of the three 30-min qualitative
searches of the bar. The diver had been in-
structed to concentrate on pustulate organisms
or species judged uncommon by our earlier
work. On the second search, he obtained eight
species, including one P. cooperianiui and two Q.
ptistulosa. During the final search he retrieved
eleven species, including two P. cooperianus and
two Q. pustulosa. The Orange-footed Pimple-
back was not found with the brail, on any of the
shoreline searches, or in the quadrat samples.
Conchological data on the three live P.
cooperianus are as follows:
Length (mm) Height (mm.) Width (mm)
74 63 37
68 60 38
71 64 42
By gently prying the valves apart, it was ob-
served that soft tissues were healthy looking
and certainly not moribund.
Discussion
This gravel bar was dominated both in num-
bers and biomass by Corbicula; evidently this
had no effect on the unionids or P. cooperianus.
In addition, it appears that requirements for
food, water quality, and substrate for adult P.
cooperianus must differ very little from the 25
other unionids inhabiting this bed. In a study of
21 species in Michigan streams, Strayer (1983)
concluded that microhabitat differences were
not discernible for 21 of the unionids. In addi-
tion, two other species, the fairly uncommon
Vol. 100(1)
January 31, 1986
THE NAUTILUS 17
Cumberlandia monodonta and the endangered
Lampsiliti higginsi, have also been collected
from very diverse and densely populated mussel
beds in the Upper Mississippi River. Cumber-
landia monodonta was usually taken in samples
where 50% of the sites had at least 20 species of
common or wide-ranging mussels. Lampsilis
higginsi was in association with 17 or more com-
mon unionids at 50% of the reported sites in the
upper Mississippi River (Nelson and Freitag
1979).
Wilson and Clark (1914) judged P. cooperia-
nus to be "not rare" during their survey of the
Cumberland River. However, Neel and Allen
(1964) were unable to locate this species during
a follow-up study on the same river. It is ap-
parent that the historical range of P. cooperia-
nus has diminished and the species is in danger
of becoming e.xtinct. Some of the reasons often
cited for the loss of mussels in large rivers in-
clude: sedimentation, navigation activities,
pollution, reservoir construction (many with
deoxygenated, low pH, and cold water releases),
and loss of fish hosts (Fuller 1974).
Conversion of large, free-flowing rivers such
as the Ohio to navigable waterways altered the
habitats of many benthic organisms. However,
some extensive areas with suitable substrate,
flow, water quality, and nutrients still exist
which support recruiting unionid communities.
For the endangered P. cooperianus, the studied
gravel bar on the Ohio River appears to meet
requirements necessary for maintenance of
adults.
The range reduction for P. cooperianus is
probably related to species-specific problems of
reproduction or recruitment. Conversion of the
Ohio River from a freely-flowing river to a con-
trolled waterway probably modified the avail-
able habitats and could have had detrimental
effects on host fish. However, it is also possible
that this species is slightly more sensitive to
altered habitats than the other thick-shelled
unionids at the mussel bed. Perhaps conditions
have degraded to a point that P. cooperianus
can maintain itself but does not possess energy
reserves necessary for production of adequate
numbers of glochidia.
Similar problems may also be blamed for loss
of species in the genus Dysnamia, which were
once commonly collected in riffles or shoals in
large rivers (Stansbery 1970). Riffle and shoal
habitats are now almost non-existent in large
rivers in North America; their disappearance
could be blamed for loss of recruiting popula-
tions oi Dysnotnia and Plethobasus.
A possible solution for long-term maintenance
of P. cooperianus is artificial propagation (Isom
and Hudson 1982) and translocation of im-
mature forms to suitable habitats. Projects such
as these will be important for separating direct
effects of habitat alteration from indirect effects
such as reduction in the availability of the host
fish.
Acknowledgments
Funds for this work were provided by the
Navigation Planning Support Center, U. S.
Army Engineer District, Louisville in Louisville,
Kentucky.
LITERATURE CITED
Clarke, A. H., and Fuller, S. L. H. 1983. A Field Guide to the
Endangered Mussels. Technical Report in Preparation,
U.S. Army Engineer Waterways Experiment Station,
Vicksburg, Miss.
Fuller, S. L. H. 1974. Clams and Mussels (Mollusca:
Bivalvia), In: Hart, C. W., Jr., and S. L. H. Fuller, eds..
Pollution Ecology of Fresh-Water Invertebrates. Academic
Press, New York.
Isom, B. G,, and Hudson, R. G. 1982. In vitro Culture of
Parasitic Freshwater Mussel Glochidia. The Nautilus
96(4):147-151.
Neel, J. K., and Allen, W. R. 1964. The Mussel Fauna of the
Upper Cumberland Basin Before Its Impoundment. Mala-
rologia 1:427-459.
Neff, S. E., and Pearson, W. 1980. Aquatic Ecology and
Water Quality Studies for the Lower Ohio River Naviga-
tion Study, Unpublished report submitted to the Louisville
District Office, Louisville, Ky.
Nelson, D. A., and Freitag, T. M. 1979. Ecology, Identifica-
tion, and Recent Discoveries of Higgin's Eye {Lampsilis
higginsi]. Spectacle Case (Cumberlandia monodonta). and
Fat Pocketbook (Potamiius capax) Mussels in the Upper
Mississippi River. In: Rasmussen, J. L., ed., Proceedings of
the UMRCC Symposium on Upper Mississippi River
Bivalve Mollusks. J. L. Rasmussen, ed. pp. 120-145.
Stansbery, D. H. 1970. Eastern Freshwater Mollusks (I) The
Mississippi and St. Lawrence River Systems. Malacologia
10(l):9-22.
Strayer, D. L. 1983. Notes on the Microhabitats of Unionid
Mussels in Some Michigan Streams. Amer. Midi Nat.
106(2):411-415.
Wilson, C. B., and Clark, H. W. 1914. The Mussels of the
Cumberland River and Its Tributaries. Report U. S. Com-
mission Fisheries for 1912 and Spec. Papers, pp. 1-63
(separately issued as Bureau Fisheries Document No. 781).
Williams, J. C. 1969. Mussel Fishery Investigation, Ten-
18 THE NAUTILUS
January 31, 1986
Vol. 100(1)
nessee, Ohio, ;ind (Sreen Rivers. Final Report. State of
Kentucky Project Number 4-19-R, Report to U. S. Fish
and Wildlife Service, 107 pp.
Williams, J. C, and Schuster, G. A. 1982. Fresh-Water
Mussel Investigations of the Ohio River, Mile 317.0 to Mile
981.0, Report Submitted to the U. S. Army Engineer Dis-
trict, Louisville; Kentucky Department of Fish and Wild-
life Resources; Division of Fisheries, U. S. Fish and Wild-
life Service, Areas 3 and 4.
CHARACTERIZATION OF A BIVALVE COMMUNITY IN THE
TANGIPAHOA RIVER, MISSISSIPPI
Andrew C. Miller
Barry S. Payne
Environmental Laboratory
U.S. Army Engineer Waterways Exp. Station
P.O. Box 631, Vicksburg, MS 39180
and David W. Aldridge
Department of Biology
North Carolina A&T State University
Greensboro, NC 27411
ABSTRACT
On 5 July 1983 a quantitative collection of bivalves was made at the Tangipahoa
River in southern Mississippi. Although the river water was extremely soft and
the substrate and water quality were good, a diverse and healthy mollv^k com-
munity was found. In addition to the Asian Clam. Corbicula, five species of
unionids fFusconaia flava, Quadrula pustulosa, Elliptic crassidens, Tritogonia
verrucosa and Villosa sp.J were taken. Numerically, Corbicula (8.93/m.^), out-
numbered total unionids (1.2Jt/m.'). However the dominant feature of the benthic
biomass were the unionids with a total tissue dry mass of 170^.5 m.g/m' as com-
pared with 1015.0 mglm} for Corbicula.
habitats. The purpose of this research was to
characterize, using quantitative field and
laboratory techniques, a bivalve community in
the Tangipahoa River in southern Mississippi.
Mississippi bivalves were first investigated by
Hinkley (1906), later by Grantham (1969), and
then Stern (1976) who concentrated on the
unionids of the Lake Maurepas-Pontchartrain-
Borgene drainage system. Recent mollusk
studies in Mississippi include an investigation
of mussels in the Big Black River (Hartfield
and Rummel 1984), distribution of Corbicula
(Hartfield and Cooper 1983), and a discussion of
diversity and abundance of mussels in the south-
west portion of the state (Hartfield and Ebert
1984). The above-cited studies, while providing
useful information on species composition and
ecology, have been directed toward qualitative
assessments of the molluscan fauna. Quantita-
tive unionid studies, either in Mississippi or
other parts of the country, are relatively uncom-
mon. The primary reason for this is the diffi-
culty of collecting significant numbers of live
mussels from a measured area. Benthic grab
samplers usually do not retrieve enough sub-
strate to provide reliable population estimates;
in addition, they do not function well in gravel
Study Area
The Tangipahoa River originates in Lincoln
County, flows south through Amite and Pike
counties, then enters Lake Tangipahoa approxi-
mately 4 miles southeast of McComb in southern
Mississippi. Below Lake Tangipahoa the river
flows in an easterly direction into Louisiana and
ultimately enters Lake Pontchartrain near New
Orleans. The study site (latitude 31°07'15"N.,
longitude 90°29'25"W., elevation 85.3 M. Mc-
Comb S, Miss., US Geological Survey Quad-
rangle) was located south of Lake Tangipahoa
and 2 miles south of the town of Magnolia. In
this area the river consisted of pools, riffles, and
runs with steep, partially eroding banks.
Canopy cover was usually complete and sur-
rounding land was either undeveloped riparian
forest or pasture. At the time of collection the
Vol. 100(1)
January 31, 1986
THE NAUTILUS 19
water depth was no greater than 1.0 m, except
in pools, and widths ranged from 4 to 10 m.
Based upon preliminary surveys, this site was
judged to be one of the richest for bivalves when
compared with adjacent rivers or other portions
of the Tangipahoa River.
Substrate at the study site consisted of gravel-
ly sands. On 5 July 1983 chemical conditions of
the river water were as follows: calcium hard-
ness, 3.2 mg/1; pH, 6.8; and turbidity, 8.9 NTU.
On 12 August at 1300 hr the air temperature
was 27°C and water temperature was 24°C.
Additional chemical data from the Tangipahoa
River at Hwy 190 in Louisiana (taken from the
Louisiana Stream Control Commission as cited
by Stern 1976) further characterize this river as
clear, well oxygenated, and with low dissolved
solids and turbidity.
Methods and Materials
Mollusks were collected from two adjacent
riffles by two workers during a 6-hr period on 5
July 1983. Unionids were obtained from both
sites (214 m^) and Corbicula were taken only
from a subsection of the downriver site (44 m^).
Bivalves were the dominant feature of the com-
munity; no snails or fingernail clams and only a
few immature insects were collected. Collec-
tions were made by hand or with a basket
dredge, an open-ended wire basket that was
pulled through the substrate and retained only
objects equal to or greater than 1 cm in dia-
meter. All mollusks were kept cool and returned
to the laboratory alive. The majority of the
specimens were used in a series of laboratory
experiments on navigation effects that were
part of the Environmental and Water Quality
Operational Studies at the Waterways Experi-
ment Station.
In the laboratory, total shell length and height
were recorded. Anterior and posterior mussels
were cut with a scalpel or small knife and the
viscera removed. Shells and viscera were dried
for 24-48 hr at 75 °C before weighing to the
nearest 0.1 mg on a Mettler balance. Regression
equations for length, height, or tissue dry mass
(TDM) were derived after transforming data to
logio or logj with an IBM 4331 computer using
the Statistical Analysis System.
Results and Discussion
At the study area on the Tangipahoa River,
Corbicula, which was common in Mississippi by
the late 1960's (Grantham 1969), represented
87.8% of the total bivalve fauna (Table 1). Asian
Clams were common throughout the downriver
site, even in shallow water on unanchored sands
where unionids were never collected. Length-
frequency analysis (Fig. 1) indicated that two
major cohorts were present in early July. About
40% of the Corbicula were approximately
14-mm long; the second cohort ranged from 20
to 30 mm. Based on Corbicula collections made
in May in the Altamaha River, Georgia, Sickle
(1979) identified a cohort at 14 mm and a second
at 22 mm. In that river the first year spawn had
achieved 4 mm by August of the same year. In
the Tangipahoa River the second year cohort
was more slow growing and exhibited a wider
range of lengths than did the first year group,
findings which are consistent with Sickle (1979).
A power curve (Fig. 2) provided the highest r^
value for the relationship between shell length
and TDM. Sickle (1979) concluded that the rela-
TABLE 1. Summary
statistics for bivalves collected from two
adjacent sites on
the Tangipahoa River
Pil^eC
3unty,
Mississippi, 5 July 1983.
Total
Numbers
Tissue
TDM/m^
1015.0
Dry
Mass
%
37.3
Shell Len
gth, mm
Species
No.
Collected
393
No./m
8.93
%
87.8
X
21.6
CV*
23.6
min
10.0
max
Corbiau la
33.0
Fueconaia flava
158
0.74
7.3
531.1
19.5
46.0
16.1
31.3
70.0
Quadrula pustulosa
55
0.26
2.5
296.8
10.9
47.6
11.8
36.6
64.2
Eltiptio crassidens
31
0. U
1.4
605.5
22.3
105.9
10.9
84.0
126.0
Tritogonia vevruoosa
18
0.08
0.8
271.1
10.0
94.0
13.1
69.0
108.0
Villoea sp.
4
0.02
0.2
-
-
52.9
15.3
43.8
61.1
Total unionids
266
1.24
12.2
1704.5
62.7
Total bivalves
659
10. 17
2719.5
Coefficient of variation
20 THE NAUTILUS
January 81, 1986
Vol. 100(1)
CORBICULA
Lr
15 20
SHELL LENGTH. MM
FK;. 1. Shell length-frequency distributions for Corhiaila
collected from the Tangipahoa River. Pike County.
Mississippi.
400
300
2001-
100
80
60
40
CO
20
GO
S2 10
CORBICULA
Y = 0.0047 X3 21 r2 = 0.97
_L
J L
J
12 5 10
SHELL LENGTH. MIVI
15 20 30 40
FIG. 2. Relationship between tissue dry mass and shell
length for CorbicuUi collected from the Tangipahoa River.
Pike County, Mississippi.
>-
CJ
a
LU
az
30 r
25
20 h
15
10
o
ac
>■
o
a
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QUADRULA
PUSTULOSA
tfk
0 20 30 40 50 60 70
SHELL LENGTH, MM
17
15 h
10
0
^
FUSCONAIA
FLAVA
EL
0 30 40 50 60 70 80
SHELL LENGTH, MM
25 r
20
15 h
10
5
0 Uj 1 III I"
TRITOGONIA
VERRUCOSA
0 50 60 70 80 90 100 110
SHELL LENGTH, MM
15 r
10
ELLIPTIO
CRASSIDENS
0 80 90 100 110 120 130
SHELL LENGTH, MM
FIC. 3. Shell length-frequency distributions for four species
of mussels collected from the Tangi[)ahoa River. Pike
County, Mississippi.
Vol. 100(1)
January 31, 1986
THE NAUTILUS 21
tionship between length and TDM was best
described with a power curve for Altamaha
River fauna and collections made in the Mud
River, West Virginia, by Joy and McCoy (1975).
Although Corhicula numerically dominated the
Tangipahoa River bivalve community, because
of their smaller size they constituted only 37.3%
of the total molluscan TDM (Table 1).
Ficsconaia Jlava' , a widely distributed unionid
in southern Mississippi and Louisiana (Stern
1976), was the most abundant unionid in the
Tangipahoa River with densities equal to
0.74/m^ The second most abundant species,
Quadrula pustulosa. (this southern form called
refidgens Lea by some) has been collected in
mud, sand, and gravel substrate in flowing and
slack water habitats in this region (Stern 1976).
Total shell length for F. Jlava ranged from 31.3
to 70.0 mm; length-frequency distributions (Fig.
3) suggest that a major cohort existed from 36
to 44 mm. For Q. pustulosa a cohort was identi-
fied at approximately 45 mm with at least one
below and possibly two cohorts above this
range. For both of these Tangipahoa River
unionids, the highest r' for length and TDM was
'Alias cerina Conrad. 1838. See Hartfield and Rummel
(198.5).
a function of X' (Fig. 4). Quadrula pustulosa ex-
hibited a slightly higher ratio of TDM to shell
length, an indication of greater tissue mass com-
pared to length of shell, than did F. flava. While
F. JJava and Q. pustulosa comprised only 7.3%
and 2.5% of the bivalve community, because of
their larger size they represented 19.5% and
10.9% of the total bivalve TDM, respectively.
While Elliptio crassidens and Tritogonia ver-
rucosa exhibited densities of 0.14 and 0.08/m^
respectively, the contribution of these larger
bivalves to the total TDM was approximately
equal to that of the previous two species (22.3%
and 10.0%, respectively). Grantham (1969)
reported that the former species had sporadic
distribution in Mississippi, and Stern (1979)
found E. crassidens common in headwater
streams in this region. Average shell length of
E. crassidens (105.9 mm) exceeded that for T.
verrucosa (94.0 mm) by approximately 10%. A
linear plot of total shell length to total shell
height (Fig. 5) demonstrated a greater ratio of
height to length for E. crassidens then T. verru-
cosa at sizes greater than 97 mm. For individ-
uals larger than 97 mm, the reverse was true;
height to length was greater for T. verrucosa
than for E. crassidens.
In this section of the Tangipahoa River, F.
2250
2000
1750
1500
1250
1000
750
500
250
QUADRULA PUSTULOSA
Y = 0.68 X2 - 411.4, r2 = 0.86
FISCONAIA FLAVA
•• ,,^., •.: Y = 0.52 X2 - 416.1. r2 = 0.82
^,l-J I I I I I I I
_L
0 32 34 36 38 40 42 44 46 48 50 52 54 56 58 60 62 64 66 68
SHELL LENGTH. MM
FIG. 4. Relationship between tissue dry mass and shell length for Q. fnistulosa and F.Jhim collected
from the Tangipahoa River, Pike County, Mississippi.
22 THE NAUTILUS
80 -
70 -
s 60 -
S 50
OD 40
30
20
January 81, 1986
ELUPTIO CRASSIDENS
Y = 0.46X + 12.3. r2 = 0.76
Vol. 100(1)
TRITOGONIA VERRUCOSA
Y = 0.68X - 11.7. r2 = 0.90
h^
_L
_L
_L
_L
_L
50
60
110
120
130
70 80 90 100
SHELL LENGTH. MIVI
FIG. .5. Relationship between shell height and shell length for E. crassideiis and T. verrucosa col
lected from Tangipahoa River, Pike County, Mississippi.
flava, because of its numbers, and E. crassidens.
because of its size, dominated the unionid TDM.
The other three unionids, Q. pustulosa, T. verru-
cosa, and Villosa sp., were a minor part of the
unionid community. While the unionids domi-
nated the bivalve biomass (62.7%), they were
outnumbered by Corbicula (87.8%). In addition,
the Asian clams, because of their rapid growth
rates, exhibited higher productivity in terms of
tissue growth per unit time than did the
unionids.
Since dissolved calcium is of obvious impor-
tance for shell maintenance, it is significant that
the Tangipahoa River supported a healthy com-
munity regardless of soft water (3.2mg/( as
CaCOj). In central New York, Clarke and Berg
(19.59) collected no unionids in water with total
alkalinity less than 47 ppm. Harman (1969)
found unionids in water with total alkalinity
ranging between 20 and 30 mg/f and stated that
sudden changes in pH were probably more detri-
mental than low dissolved solids. Tangipahoa
River fauna live in water at the extreme lower
end of the range of dissolved calcium concentra-
tions usually reported for the freshwater
Mollusca.
A site on the Tangipahoa River in southern
Mississippi was identified which supported a
dense, fairly diverse mollusk community.
Bivalves were found in good quality substrate in
water that was clear, well oxygenated but with
extremely low dissolved calcium levels. While
freshwater mollusks are usually found in
medium to hardwater habitats, it appears that
reduced dissolved calcium concentrations are
not limiting the Tangipahoa River fauna.
LITERATURE CITED
Clarke. A. H., Jr. and Berg, C. 0, 19.59. The Freshwater
Mussels of Central New York, with an Illustrated Key to
the Species of Northeastern North America. University
Agricultural Experiment Station Memoir 367:1-79.
Grantham, B. J. 1969. The Freshwater Pelecypod Fauna of
Mississippi, Doctoral Dissertation, University of Southern
Mississippi, Hattiesburg, Miss.
Harman. W. N. 1969. The Effect of Changing pH on the
Unionidae. The Nautilus 83:69-70.
Hartfield, P. D. and Cooper, C. M. 1983. Distribution of
Corbicula Jluminea the Asiatic Clam, in Mississippi. The
Nautilus 97:66-68.
Hartfield, P. D. and Ebert, D. 1984. Factors Affecting the
Diversity and Abundance of Mussels in Southwest Missis-
sippi. Presentation for Mississippi Academy of Sciences,
Biloxi, Miss., March 1984.
Hartfield, P. D. and Rummel, R. G. 198,5. Freshwater
Mussels (Unionidae) of the Big Black River, Mississippi.
The Nautilus 99(4):\\6-\l9.
Hiiikley, A. A. 1906. Some Shells from Mississippi and
Alabama. The Nautilus 20:52-55.
Vol. 100(1)
January 31, 1986
THE NAUTILUS 23
Joy, J. E. and McCoy, L. E. 1975. Comparison of Shell
Dimensions and Viscera Mass Weights in Corbicula
manilensis (Philippi, 1844). The Nautilus 89(2):51-54.
Sickle, J. B. 1979. Population Dynamics of Corbicula in the
Altamaha River, Georgia. In J. C. Britton, ed., Proceed-
ings. First International Corbicula Symposium, The
Texas Christian University Research Foundation, Ft.
Worth, Texas.
Stern, E. M. 1976. The Freshwater Mussels (Unionidae) of
the Lake Maurepas-Pontchartrain-Borgne Drainage Sys-
tem, Louisiana and Mississippi. Ph.D. Thesis, Louisiana
State University, Baton Rouge, La.
NOTES ON SPECIES OF BROCCHINIA
(GASTROPODA: CANCELLARIIDAE)
Richard E. Petit'
Research Associate
Department of Invertebrate Zoology
National Museum of Natural History
Smithsonian Institution
Washington, D.C. 20560
ABSTRACT
Available replacement names are discussed for Voluta mitraeformis Brocchi,
181Jt, the type species of Brocchinia Jousseaume, 1887, and a primary junior
homonym of Voluta mitraeformis Lamarck, 1811. Cancellaria pusilla Adams,
1869 is also preoccupied. This Recent species is redescribed as Brocchinia clenchi,
n. sp.
Voluta mitraeformis Brocchi, 1814, a well-
known cancellariid of the European Tertiary,
is the type species of the genus Brocchinia
Jousseaume, 1887. Although this taxon is fre-
quently cited, its status as a junior primary
homonym of Voluta mitraeformis Lamarck,
1811 has been noted in the literature only by
Malatesta (1974:376) and DavoH (1982:61).
Malatesta (1974:377) considered Cancellaria
pusilla H. Adams, 1869 to be available as a
replacement name for the preoccupied Voluta
mitraeformis Brocchi, although he considered
the Recent and Tertiary populations to be sepa-
rable. He further stated that the "fossil sub-
species" {sotfospecie fossile) had as an available
name Cancellaria cerithiopsis Almera & Bofill,
1887 {sic). Malatesta's conclusions are incorrect
as C. pusilla H. Adams is not an available name,
being a junior primary homonym of Cancellaria
pusilla Sowerby, 1832, and C. cerithiopsis
'Mailing address: P.O. Box 30, North Myrtle Beach, SC
29582.
Almera & Bofill dates from 1898, not 1887.
Earlier synonyms of V. mitraeformis Brocchi
exist, as shown below.
Davoli (1982:61) stated that Voluta mitrae-
formis Brocchi, 1814 and Voluta mitraeformis
Lamarck, 1811 should not be regarded as pri-
mary homonyms inasmuch as Brocchi pointed
out that his species belonged to Lamarck's
genus Cancellaria. Davoli referred to the
Preamble of the International Code of Zoologi-
cal Nomenclature in his plea for retention of
Brocchi's V. mitraefoifmis, but the applicable
portion of the Code in this instance is Article
60a which states: "A junior homonym must be
rejected . . ." (italics added). This is unequivocal.
Brocchinia Jousseaume, 1887
Type, by subsequent designation of Sacco, 1894, Brocchi-
nia mitraeformis (Brocchi) ( = Voluta mitraeformis Brocchi,
1814 non Voluta mitraeformis Lamarck, 1811; = Brocchinia
parvula tauropama Sacco, 1894).
Brocchinia has been cited as a subgenus of
Narona H. & A. Adams, 1854 by various
authors (see synonymy in Malatesta, 1974:377).
24 THE NAUTILUS
January 31, 1986
Vol. 100(1)
The type of Narona is Cancellaria clavaiula
Sowerby, 1832 from the tropical eastern Pacific.
There is no evidence for a subgeneric relation-
ship between the two genus-level taxa. Narona
is characterized by a somewhat tabulate shell
having a distinct anterior canal; its columella
bears two strong, sharp folds, the posterior one
being superior. Brocchinia has a small non-
tabulate shell with a rounded anterior; the short
siphonal canal evidenced only as a slight curving
of the columella; its two columellar folds are
weak and rounded.
Brocchinia parvula parinila (Beyrich, 1856)
Synoyiymy-
Cancdlaria parvula Beyrich, 18.56:58, pi. 3, figs. 82a-b.
Cancellaria bicarinata Homes & Auinger, 1890:281, pi. 33,
figs. 16a-c.
Brocchinia mitraefnrmis parvula (Beyrich), .Jansseii,
1983:9, pi. 1, figs.' 5-7; pi. 5, fig. 3, text-fig. 4.
Cancellaria parvula Beyrich is apparently
the earliest named taxon considered to be a
synonym or subspecies of Valuta vfiitraeformis
Brocchi, and therefore becomes the nominotypi-
cal subspecies of the species group (I. C.Z.N.
Article 47). This German Miocene species was
cited by Gilbert (1952:130, pi. 9, fig. 16; 1960:4)
as a form of C. mitraeformis (Brocchi), his
figure agreeing well with Beyrich's original
figures. Brocchinia parvula has been treated as
a valid species, separable from B. mitraeformis.
by Kautsky (1925:137), Sacco (1894:70) and
Seiber (1936:93). Davoli (1982:61) mentions C.
parvula in his discussion but does not include it
in his synonymy of B. mitraeformis. Malatesta
(1974:376), in his synonymy, lists Kautsky's cita-
tion of B. panmla but does not list the original
description, a possible indication that he consid-
ered the two to be separable. In the most recent
paper treating the subject, Janssen (1983:9, 10)
considers B. parvula to be a subspecies of.S.
mitraeformis (Brocchi) and states that B. par-
vula occurs in the Mediterranean Pliocene as
well as in the northern European Miocene. This
interpretation of the relationship between B.
parvula and B. mitraeformis agrees with this
writer's opinion.
Brocchinia parvula tauroparva Sacco, 1894
Synonymy -
Volula milraiiformis Brocchi, 1814:fi45, pi. 15, fig. 13 (noii
Valuta mitraeformis Lamarck, 1811:73).
Brocchinia ynitraeformix var. tauroparva Sacco, 1894:68,
pi. 3, fig. 82.
Narona (Brocchinia) mitraejhi-viis (Brocchi), Davoli, 1982:
61, pi. 7, figs. 3-6.
Sacco (1894:68-70) named eight varieties
of Brocchinia mitraeformis (Brocchi) from
the Italian Pliocene. The first of these, Broc-
chinia mitraeformis tauroparva. is not distinct
from the typical form, and is here considered to
be a subjective synonym of B. mitraeformis
(Brocchi). Brocchinia tauroparva (Sacco) thus
replaces the preoccupied V. mitraeformis
Brocchi.
Brocchinia clenchi, n. sp.
' Figs. 1-4
Synonymy -
Cancellaria pufiiJla H. Adams, 1869:274, pi. 19, fig. ]2(non
Cancellaria puxilla Sowerby. 1832:6, fig. 34).
Cancellaria mitraeformis Brocchi, .Jeffreys, 1885:49.
Narona (Brocchinia) p^isilla (H. Adams), Nordsieck, 1968:
151, pi. 25, fig. 87.,3().
Df'.srnj9^iOK-Paucispiral nucleus smooth,
heliciform, consisting of about IV2 whorls; tran-
sition from protoconch to teleoconch almost im-
perceptible. Faint peripheral spiral cords arise
midway on the first postnuclear whorl. The
spiral sculpture consists of 3 to 5 extremely
weak cords, with 3 usually visible on the spire
whorls, and 5 or so on the body whorl. Axial
sculpture, when present, consists only of weak
nodes on the periphery that are crossed by the
spiral cords. Suture distinct, slightly impressed.
Teleoconch of about 4 whorls; nonumbilicate.
Aperture ovate with a weak but noticeable col-
umellar callus. Columella with two distinct,
rounded folds of approximately equal size, the
posterior one being slightly larger and more
pronounced. Siphonal canal indicated by the
angled base of the columella and a minute
depression in the base of the aperture. Outer lip
prosocline, usually denticulate within. The den-
ticles, which do not extend to the edge of the lip,
vary in strength and number. Shell white or
horn colored. Animal unknown.
Type Material: Holotype, 4.5 mm x 2.3 mm
(USNM 849002); Paratype, 5.2 mm x 2.6 mm
(USNM 189694); Paratype, BM(NH) 1855.4.
4.202, 6.0 mm x 2.5 mm (possibly the type of C.
pu.'iilla Adams).
Type locality: Josephine Bank, 340-430 fms.
Josephine Bank is situated at approximately
Vol. 100(1)
January 31, 1986
THE NAUTILUS 25
FIGS. 1-4. Brricrhima rlenchi new species. 1, Paratype, BM(NH) 185.S.4.4.202, Oratova, Canary
Islands. 15x. 2. Paratype, USNM 189694, Josephine Bank, 621-786 m, 20x. 3, Holotype, USNM
849002, Josephine Bank, 621-786 m, 20 x. 4, Apical view of protoconch of holotype, 65 x.
37°N, 14°W, due West of the southern tip of
Portugal. The type and paratype in the USNM
are from the Jeffrey's collection.
Etymology: This species is respectfully dedi-
cated to the memory of the late Dr. William J.
Clench.
Discussion: This Recent species was previous-
ly described as Cancellaria pusilla Adams,
1869, but that name is preoccupied by C. pusilla
Sowerby, 1832. Jeffreys (1885:49) placed C.
pusilla Adams in the synonymy of C. rnitrae-
formis (Brocchi), while Sykes (1911:332),
Harmer (1918:396) and Dautzenberg (1927:73)
considered the Recent species to be distinct.
The Recent B. clenchi is easily separable from
the Tertiary species by its much smaller size and
by its comparatively weak sculpture. The illus-
tration accompanying Adams' description of C.
pusilla is misleading, as the fine, almost in-
distinct spirals are shown to be quite strong.
26 THE NAUTILUS
January 31, 1986
Vol. 100(1)
The drawings of Nordsieck (1968:pl. 25, fig.
87.30; 1979:pl. 37, fig. 6) are too poor to be
recognizable. Although included by Nordsieck &
Talavera (1979:152) with the notation that its
occurrence in the Canaries may be accidental,
specimens have now been found in fish traps in
Tenerife South at a depth of 43 m (Talavera,
pers. comm.).
As the type of C. piisilla Adams cannot be
positively identified, the species has been re-
described so that a holotype can be designated,
rather than simply proposing a nomen novum.
The BM(NH) specimen listed as a paratype is
from the R. M. McAndrew collection.
Acknowledgments
This paper would not have been possible with-
out considerable assistance. Dr. Franco Davoli,
Universita di Modena, Italy, furnished a transla-
tion of his work, and corresponded regarding
the desirability of retaining Brocchi's taxon. Mr.
Piero Piani, Bologna, Italy, furnished transla-
tions, comments and literature.
Mrs. Kathie Way, British Museum (Natural
History), London, located the possible type of
Adams' C. pusilla and made it available for
study.
The late Dr. Joseph Rosewater, National
Museum of Natural History, Washington, D.C.,
made the Jeffreys specimens available and
located pertinent references.
Dr. Francisco G. Talavera, Museo Insular de
Ciencias, Tenerife, Canary Islands, furnished in-
formation and literature.
Dr. A. G. Beu, N.Z. Geological Survey, Lower
Hutt, New Zealand, read and commented on an
early draft of this paper.
Dr. M. G. Harasewych, National Museum of
Natural History, Washington, D.C. made the
photographs, prepared the plate, and reviewed
the manuscript.
The cooperation and assistance of all is grate-
fully acknowledged.
LITERATURE CITED
Adams. H. 1869. Descriptions of a new genus and fourteen
new species of marine shells. Froc. Zool. Soc. Loiidtni.
1869^112-21^, pi. 19.
Adams, H. & A. 1853-1858. The genera uf Recent Mollusca.
3 vols. London.
Almera, J. & A. Bofill. 1898. Moluscos fosiles recogidos en
los terrenos pliocenicos de Cataluna. Bol. Com. Mapa
geoL Espana. IV (ser. 2): XII + 223, 14 pis., Madrid.
Beyrich, E. 1856. Die Konchylien des norddeutschen Ter-
tiargebirges. Zeitschr. d. Deutsch. geol. Ges. 8.
Brocchi, G. B. 1814. Conchiologia fossile subappenniria con
osservazioni geotogirhe sugli Appenniyii. 2 vols.,
Stamperia Reale, Milano.
Dautzenberg, Ph. 1927. Mollusques provenant des cam-
pagnes scientifiques du Prince Ibert I de Monaco dans
rOcean Atlantique et le Golfe de Gascogne. Result.
Camp. Scient. Pr. Alberta I de Monaco, fasc. LXXII,
400 pp., 9 pis.
Davoli, F. 1982. Cancellariidae (Gastropoda). In E. Monta-
naro Gallitelli (ed.). Studi monografici sulla malacologia
mioceniea modenese. Parte I - I Molluschi tortoniani di
Montegibbio. Pobieont. Ital 72 (n.ser. vol. 42);5-73, 7 pis.,
Pisa.
Glibert, M. 1952. Faune malacologique du Miocene de la
Belgique. II. Gastropods. Inst. Roy. Sci. Nat. Belg., Mem.
121:1-197, 10 pis.
1960. Gastropodes du Diestien. du Scaldisien et
du Merxemien de la Belgique. 4me Note. Inst. Roy. Sci.
Nat. Belg.. Bull. 36(33): 1-44, 2 pis.
Harmer, F. W. 1918. The Pliocene Mollusca of Great Britain.
Part III. Pnheontographical Soc. 70:303-461. pis. 33-44.
Horncs, R. & M. Auinger. 1890. Die Gastropoden der
Meeres-Ablagerungen der ersten und zweiten Miocanen
Mediterranstufe in der ostereich-ungarischen Monarchie.
Abhdlg. Geol. Reichsanst. 6.
International Commission on Zoological Nomenclature.
1985. International Code of Zoological Nomenclature,
3rd Ed. pp. i-xx, 1-338. London.
Janssen, A. W. 1983. An account of the Cancellariidae
(Gastropoda) of Winterswijk-Miste (Miocene. Hemoorian),
The Netherlands. Scripta Geol. 68:1-39. 6 pis.
Jeffreys, J. G. 1885. On the Mollusca procured during the
'Lightning' and 'Porcupine' Expeditions, 1868-70. (Part
IX). Proc. Zool. Soc. London. 1885:27-63 , pis. 4-6. .
Jousseaume, F. P. 1887. La famille des Cancellariidae. Le
Natural., ami. 9. 2e ser., pp. 155-157, 163, 192-194,
213-214, 221-223.
Kautsky, F. 1925. Das Miocan von Hemmoor und Basbeck-
Osten. Abh. preuss. geol. LandesanM.. N.F. 97:1-255,
12 pis.
Lamarck, .J.B.P.A. 1811. Suite de la determination des
especes de Mollusques testaces. Valuta. Ann. Mus. Nat.
d Hist. Nat. 17:54-80.
Malatesta, A. 1974. Malacofauna pliocenica umbra. Mem.
Carta Geol. It 13:XI-i-498, 32 pis.. Roma.
Nordsieck, F. 1968. Die europaischen Meeres-Gehausesck-
necken (Prosobranrhia) com Eisnifer bis Kapverden U7id
Mittelmeer. 268 p. Gustav Fischer. Stuttgart.
Nordsieck, F. & F. G. Talavera. 1979. Moluscos Marinas
de Canarias y Madera (Gastropoda). 208 p., 46 pis.
Tenerife.
Sacco, F. 1894. I mollu.schi dei terreni terziarii del Piemonte
e Liguria. Pt. XVI (Cancellariidae). Mem. R. Accad. Sc.
Torino, Clausen Ed., 78 pp.. 3 pis.. Torino.
Sieber, R. 1936, Die Cancellariidae des niederosterreichis-
chen Mioziins. Arrhir. Mollu.fk. 68:65-115.
Sowerby, G. B. 1832-33. The Conchological Illustrations.
Cancellaria. Pts. 9-13. London. 5 pis. with explanations
-I- catalogue, 10 pp. (Pts. 9-12, figs. 1-35, published 1832;
Vol. 100 (1)
January 31, 1986
THE NAUTILUS 27
pt. 13, figs. 36-44 and catalogue published 1833).
Sykes, E. R. 1911. On the mollusca procured during the
"Porcupine" Expeditions, 1869-70. Supplemental Notes,
Part IV. Proc. Malac. Soc. London 9(6):331-348.
ON THE TYPE SPECIES OF METULA H. & A. ADAMS, 1853:
BUCCINUM CLATHRATUM A. ADAMS AND REEVE, 1850
(GASTROPODA: BUCCINIDAE)
William K. Emerson
Department of Invertebrates
American Museum of Natural History
New York, New York 10024
ABSTRACT
The type species o/Metula H. and A. Adams. 1853: Buccinum clathratum A.
Adams and Reeve, 1850 (not Kiener, 183J,, nor Anton, 1839) is determined to be
referable to Metula amosi Vanatta, 1913, from, the tropical eastern. Pacific. The
genera Acamptochetus Cossmann, 1901; Antemetula Rehder, 19J,3; and Colubra-
rina Kuroda and Habe, in Kuroda, Habe, and Oyama, 1971, are placed in the
synonymy of Metula.
The "Metula problem" has long been the con-
cern of workers dealing with these buccinid
gastropods owing to the uncertain nomencla-
tural and taxonomic status of the type species of
this genus-group taxon (E. A. Smith, 1904;
Woodring, 1928; Tomlin, 1927; Rehder, 1943;
Altena, 1949; Knudsen, 1956; Cernohorsky,
1971; Olsson and Bayer, 1972, Kilburn, 1975;
and Houbrick, 1984). This note undertakes to
solve these questions.
The type of Metula, Buccinum. clathratum
A. Adams and Reeve (1850, p. 32, pi. 11, fig.
12), was stated to have been dredged off the
Cape of Good Hope, in 136 fathoms [248 meters]
during the 1843-1846 voyage of the H.M.S.
"Samarang". TomHn (1927, p. 160), in his review
of the South American mollusks of the "St.
George" Expedition, however, noted that this
species was: "Originally described from deep
water off the Cape, but that locality, like many
others in the 'Samarang' work, is certainly
erroneous." Furthermore, Tomlin (1927, op. cit.)
concluded that this taxon was referable to speci-
mens in his collection from Balboa, Panama,
which he identified as "Metula clathrata (A. Ad.
& Rve.)". Because later workers have largely ig-
nored or questioned the identity of Buccinum
clathratum A. Adams and Reeve, 1850, the type
species oi Metula H. and A. Adams, I examined
the holotypic specimen of this taxon, which is in
the British Museum (Natural History).
The specimen labeled as holotype of Buccinum
clathratum. (BM(NH), 1874. 12. 1'l. 145; here illus-
trated, figures 1, 2) is 25.3 mm in height. The
original polychrome illustration of the type (A.
Adams and Reeve, 1850, pi. 11, fig. 12) depicts a
specimen of the same size as the holotype, which
is now faded and has a chip on the anterior por-
tion of the outer lip.
As Cernohorsky (1971, p. 149) has pointed
out, Bu.cci.num clathratum (A. Adams & Reeve,
1850) is twice preoccupied (not Kiener, 1834, p.
101, nor Anton, 1839, p. 91). Fortunately, a re-
placement name is not required, as Metula
amosi Vanatta (1913, p. 22, figs. 1, 2; Keen,
1971, p. 566, fig. 1133; Olsson and Bayer, 1972,
pp. 906, 907, figs. 1, B-D) is an available junior
synonym of this taxon. The most common of the
Panamic Metula, this species ranges offshore
from the Gulf of California to Panama Bay.
Although large specimens attain more than 44
mm in height, mature examples of M. amosi in
the American Museum of Natural History
(AMNH) collection from Mexico and Panama
28 THE NAUTILUS
.lanuarvSl, 1986
Vol. 100 (1)
are nearly as diminutive as the lioiotype of M.
clathratn. Tomiin's (1927, op. cit.) referral of
this species to Pacific Panamanian waters is
thus confirmed, and the type locality of M.
amosi is here restricted to Balboa, Bahia de
Panama.
It should be noted that Knudsen (1956, pp. 39,
40, pi. 1, fig. 1) referred a specimen dredged off
"Spanish Guinea", West Africa to Metula
clatkrata (A. Adams & Reeve, 1850) (not
Kiener, 1834, nor Anton, 1839). The specimen
figured by Knudsen is 47 mm in height (here
reproduced, fig. 3) and is referable to an uniden-
tified specimen of Metula in the AMNH collec-
tion (#198755; here illustrated, figs. 4, 5) from
"West Africa", cx-Marcel Pin collection.
Another record of this west African species,
taken in 250 meters off Dakar, Senegal (Natal
Museum J. 4152) was referred to me by Dr. R.
N. Kilburn. These specimens, however, are not
conspecific with Metula clathrata (=M. amosi
Vanatta) on the basis of the type specimen of A.
Adams and Reeve's M. clathrata (cf . figures 1 , 2
with figures 3-5), and they appear to represent a
new species. Nor is Knudsen's west African
specimen referable to Metula boswellae Kilburn
(1975, pp. 594, 595, fig. 10b, 10c), from off
"MoQamhique", East Africa. Kilburn (1975, p.
592) accepted Knudsen's (1956, op. cit.) referral
of the "Spanish Guinea" specimen to M.
clathrata (A. Adams & Reeve, 1850) and he
noted that this taxon was preoccupied. Kilburn
(1975, op. cit.), therefore, renamed this taxon,
Metula knudseni (Kilburn, 1975, p. 592). This
unnecessary replacement name thus becomes a
junior subjective synonym of Metula amosi
Vanatta, 1913.
A number of authors have discussed the taxo-
nomic status oi Metula H. and A. Adams (1853,
p. 84). Rehder (1943, p. 199) appears to be the
first to attribute Metula clathrata (A. Adams
and Reeve, 1850) as the type species (subse-
quent selection of Kobelt, 1876, p. 29, pi. 6, fig.
11 [ = "12"]). Woodring (1928, p. 286; 1964, p.
259; Keen, 1971, p. 566; Olsson and Bayer,
1972, p. 902) considered Buccinum m.etula
Hinds, 1844, to be the type species by "hidden
tautonymy," for which there is no provision in
the ICZN Code. Thus, this designation must be
rejected (Cernohorsky, 1971, p. 149). Kobelt's
(1876, op. cit.) selection oi Metula clathrata, as
the type species, therefore, appears to be the
first available designation for Metula.
Cernohorsky (1971, pp. 151, 152) and
Houbrick (1984, p. 420) considered Acampto-
chetus Cossmann (1901, p. 123) diwd Antemetula
Rehder (1943, p. 199) to be congeneric taxa. The
type species of Acamptochetus, by original
designation, is Murex mitraeformis Brocchi,
1814, from the Neogene of Italy and is a typical
Metula (Cernohorsky, 1971, fig. 46). Other
Neogene fossils are known from Europe, Java,
Sumatra, India and the Americas (Altena, 1949;
FIGS. 1-5. 1 and 2, Metula amosi Vanatta, holotype of Buccinum clathrnia A. Adams and Reeve, BM(NII) 1874. lli. I 1 . 1 4;'..
x2. 3, "Metula clathrata" after Knudsen (19.56, pi. 1, fig. 1) from "Spanish Guinea", not Metula clathrata (A. Adams and
Reeve), x IV2. 4 and 5, Metula sp., AiVINH 1987.5.5, ex-Marcel Pin coll., from "West Africa", x 1 V2.
Vol. 100(1)
January 31, 1986
THE NAUTILUS 29
Olsson and Bayer, 1972; Malatesta, 1974; and
Grecchi, 1978). The type species oi Antemetula
by original designation is Buccinum metula
Hinds, 1844. This species was originally
reported from the "West coast of Veragiia
[Republica de Panama] . . . from a depth of a few
fathoms, among mud." This locality, however, is
apparently an error, as no additional specimens
have been recognized in tropical American
waters. The type specimen (Hinds, 1844, pi. 16,
figs. 13, 14; refigured by Keen, 1971, p. 567, fig.
1134 and by Olsson and Bayer, 1972, fig. lA) is
not in the British Museum (Natural History)
teste Kathie Way, 1985). Furthermore, this
specimen could not be located there some 35
years ago (Altena, 1949, p. 385). Many years ago
Smith (1904, p. 465) noted a close resemblance
of young specimens of Metula mitreUa (A.
Adams and Reeve, 1850, p. 32, pi. 11, fig. 13,
from the "China Sea; . . . ten fathoms"), to the
illustration of the type specimen of M. metula.
Smith (1904, op. cit.) concluded that Buccinum
'metula was conspecific with B. mitrella. a well-
known Indo-West Pacific species, and that the
original west American locality was probably
erroneous. I agree with his conclusions {cf. the il-
lustration of Cernohorsky (1971, p. 150, fig. 47)
with that of Olsson and Bayer (1972, p. 905, fig.
lA). If this interpretation is correct, M. mitrella
(A. Adams and Reeve, 1850) is a junior subjec-
tive synonym of M. metula (Hinds, 1844) and
this taxon should be removed from the eastern
Pacific faunal list.
Kilburn (1975, p. 592) assigned the genus-
group name, Colubrarina Kuroda & Habe, in
Kuroda, Habe & Oyama (1971, p. 173) to the
synonymy of Metula. The type species of this
taxon by original designation is Antemetula
(Colubrarina) metulina Kuroda & Habe, in
Kuroda, Habe & Oyama, 1971 {op. cit.. p. 173,
pi. 46, fig. 9), from Honshu and Shikoku, Japan,
in 90-200 m. Described as a subgenus oiAnteyne-
tula Rehder, the type species of Colubrarina
was said to differ from the nominate subgenus
by having a larger and more coarsely sculptured
shell.
In summary, the buccinid genus Metula H.
and A. Adams, 1853, with the type species: M.
clathrata (A. Adams and Reeve, 1850) [ = M.
amosi Vanatta, 1913 (synonym; M. knu(lse7ii
Kilburn, 1975)], is available for an assemblage of
Neogene species from the Old and New World
tropical belt and for several Recent species sur-
viving in the tropics. Acamptochetus Cossmann,
1901 (type species; M. mitraeformis (Brocchi,
1814), Antemetula Rehder, 1943 (type species;
M. metula Hinds, 1844) and Colubrarina
Kuroda and Habe, 1971 (type species: M.
metulina Kuroda and Habe, 1971) are junior
synonyms.
Acknowledgments
I am very much indebted to Ms. K. M. Way of
the Department of Zoology, British Museum
(Natural History) for the loan of the holotype of
Buccinum clathratum. Dr. Richard S. Houbrick
of the National Museum of Natural History,
Smithsonian Institution kindly read a draft of
the manuscript and allowed me access to the
United States National Museum malacological
collections. I am indebted to Dr. Richard H.
Kilburn of the Natal Museum for reading the
manuscript and lending me a specimen critical
to this study. I thank Dr. Philippe Bouchet of the
Museum National d'Histoire Naturelle, Paris for
his comments on the "Metula problem".
My AMNH colleagues kindly provided valu-
able contributions as follows; Mr. Walter E.
Sage, HI, technical assistance, Mr. Peter J.
Harries, photography, and Mrs. Stephanie
Grooms, word processing.
I also wish to join others in congratulating The
Nautilus on its 100th anniversary of its found-
ing and to express my particular appreciation
of having known and benefited from the friend-
ship of three past Consulting Editors- Karl
Jacobson, Joe Rosewater and Bill Clench.
LITERATURE CITED
Adams. H. and A. 18.5.3 [-1854]. The Genera of Recent
Mollusca, Arranged According to Their Organization
London l(1.3):65-96, pis. 9-12 (June, 1853).
Adams, A. and L. Reeve. 1850. Mollusca, pt. 2:25-44,
pis. 10-17. In. The Zoology of the Voyage of H.M.S.
"Samarang". Under the Command of Captain Sir Edward
Belcher During the Years 1843-1846. London, 1848-1850.
Altena, C. 0. van Regteren. 1949. The genus. .Antemetula
Rehder in the Indo-West Pacific area, with a description
of two new fossil species. Bijdragen Tot Dierkunde 28:
385-393. 7 figs.
Anton. H. E. 1839. Verzeichniss der Conchylien welche sich
in der Sammlung von Hermann Eduard Anton befinden.
Halle, xvi -i- 110 pp.
Cernohorsky, W. O. 1971. Indo- Pacific Pisaniinae (Mollusca:
Gastropoda) and related buccinid genera. Rec. Auckland
30 THE NAUTILUS
January 31, 1986
Vol. 100(1)
Inst, and Mus. 8:131-167, 95 figs.
Cossmann, M. 1901. Essais de Paleochologie Comparee,
pt. 4, 293 pp., 10 pis.
Grecchi, G. 1978. Problems connected with the recorded
occurrence of some mollusks of Indo-Pacific affinity in
the PHocene of the Mediterranean area. Riv. Ital. Paleont.
84(3):797-812, pi. 82, 8 figs.
Hinds. R. B. 1844 [-1845], Mollusca, pt. 2, In The Zoology
of the Voyage of H.M.S. Sulphur, under the command of
Capt. Sir Edward Belcher . . . during 1836-1842. London,
pp. 25-48. pis. 8-14 (Oct. 1844).
Houbrick, R. S. 1984. A new "Metula" species from the
Indo-West Pacific (Prosobranchia: Buccinidae). Proc.
Biol. Soc, Wash. 97(2):420-424, 1 fig.
Keen, A. M. 1971. Sea Shells of Tropical West America.
Second Ed., Stanford Univ. Press, viii -^ 1064 pp., illus.
Kiener, L. C. 1834 [-1841]. Genre Buccin. In. Species
general et inconographie des coquilles vivantes . . . Paris,
vol. 9, 112 pp., 31 pis.
Kilburn, R. N. 1975. Taxonomic notes on South African
marine Mollusca (5): including descriptions of new taxa of
Rissoidae, Cerithiidae, Tonnidae, Cassididae, Buccinidae,
Fasciolariidae, Turbinellidae, Turridae, Architectoni-
cidae, Epitoniidae, Limidae, Thraciidae. Ann. Natal Mus.
22(2):577-622, 25 figs.
Knudsen, J. 1956. Marine prosobranchs of tropical West
Africa (Stenoglossa). Atlantide Report No. 4:7-110,
pis. 1-4.
Kobelt, W. 1876 [-1881]. Illustriertes Conchylienbuch,
Nurnberg, vol. 1, pp. 1-143, 50 plates.
Kuroda, T., T. Habe and K. Oyama. 1971. The Seashells of
Sagami Bay. Tokyo, 1-485 + 55 pp. (English Text),
pi. 1-22.
Malatesta, A. 1974. Malacofauna Pliocenia Umbra. Mem.
Carta Geol. Italia. Rome. vol. 13. 499 pp., 32 pis.
Olsson, A. A. and F. M. Bayer. 1972. American metulas
(Gastropoda: Buccinidae). Bull Mar. Sci. 22(4):900-925,
14 figs.
Rehder, H. A. 1943. New marine mollusks from the Antil-
lean region. Proc. U. S. Nat. Mus. 93(3161):187-203,
pis. 19, 20.
Smith, E. A. 1904. On Mollusca from the Bay of Bengal and
the Arabian Sea. In. Series III. no. 1. Natural History
Notes from H. M. Indian Survey Steamer "Investigator",
Commander T. H. Hemming, R. N. Ann. Mag. Nat. Hist.
7(13):453-473.
Tomlin, J. R. le B. 1927. The Mollusca of the "St. George"
Expedition. (I) The Pacific coast of S. America. Jour.
Conchology 18(6): 153- 170.
Vanatta, E. G. 1913. Descriptions of new species of marine
shells. Proc. Acad. Nat. Sci. Philadelphia 65(l):22-27,
3 text figs., pi. 2.
Woodring, W. P. 1928. Marine mollusks from Bowden,
Jamaica. Pt. 2. Gastropods and discussion of results.
Carnegie Inst. Washington, Pub. no. 385, vii + 564,
pis. 1-4, 3 figs.
1964. Geology and Paleontology of Canal Zone
and adjoining parts of Panama. Description of Tertiary
mollusks (Gastropods: Columbellidae to Volutidae). U.S.
Geol. Surv. Prof. Pap. 306-C:241-297, pis. 39-47.
SOME ADDITIONAL TAXONOMIC UNITS THAT FIRST APPEAR
IN PUBLICATIONS BY J. G. COOPER
Eugene Coan
Research Associate
Department of Invertebrate Zoology
California Academy of Sciences
San Francisco, CA 94118
ABSTRACT
Seventeen taxonomic units that first appeared in publications by James
Graham Cooper and that were not given in my earlier table of his taxa are listed
here. All but three are nomina nuda.
It is said that the more complete a list is, the
more glaring are its omissions. So it is, perhaps,
with my listing of the taxonomic units that first
appeared in the publications of James Graham
Cooper (Coan, 1982:148-185). Seventeen names
that should have been in that list have come to
my attention since my book was published. Most
of them were well hidden, being credited to
other workers. Fourteen of these names are
nomina nuda, only three actually being
validated by Cooper. Two replace previous
homonyms. The third is a synonymous generic
unit. It is not impossible that other similarly
hidden taxa will come to light in the future.
Vol. lOU(l)
January 31, 1986
THE NAUTILUS 31
In the listing of mollusks below, I follow the
format used in my previous table. The Cooper
papers cited refer to the Literature Cited of this
article, but I also provide, in brackets,
references keyed to the complete bibliography
of Cooper's papers given in my book (Coan,
1982:223-281).
Class Bivalvia
heringi. Thracia - Cooper, 1894 [18;)4b|: Suppl., 12th sheet,
ex Dall MS [nomen nuduvi]. Later validated by Dall, 1915:
442.
compacta. Sanguinolaria - Cooper, 1894 [1894b]: 126th
sheet [nowen nudum]. Not subsequently validated.
romijlectens. Tellina - Cooper, 1894 [1894b]: Add. & Corr.,
4th sheet, ex Carpenter MS [nomev nudum]. Not sub-
sequently validated.
Philohrya - Cooper, 1867 [1867b]: 12, ex Carpenter MS.
Type Species - Bryophila .-ietosii Carpenter, 1864a: 314,
by monotypy.
Remarks - Bi-yophila Carpenter, 1864a:314, proved to be
a homonym (reon Treitschke, 1825;.57), and Carpenter him-
self later renamed it as P/ii7obn/a (Carpenter, 1872: index, p.
21). By then, however, it was too late; Cooper had already
validated the name. Cooper did not expressly propose
Philohrya as a replacement name and it must therefore be
taken as a new genus.
Class Gastropoda
bimaculata Clypidella - Cooper, 1867 11867b]: 24, ex Dall
MS ]noinen nudum]. Later validated by Dall, 1871:132;
160; pit. 15, fig. 7), as Fissurellidaea bimaculata.
callomarginata. Clypidella - Cooper, 1867 [1867b]: 24, ex
Carpenter MS ]nomen nudum]. Later validated by Dall,
1871:133; 160; pit. 15, fig. 8.
clathftita. Ocinebra interfossa "var." - Cooper, 1870
[1870f]:69, ex Carpenter MS [nomen nudum]. Later vali-
dated by Dall, 1919:334, as Tritonalia interjmsa
clathrata.
compactum. Buccinum - Cooper, 1894 ]1894b]: 15th sheet,
ex Dall MS [noinen nudum]. Not subsequently validated.
gabbiana. Chemnitzia - Cooper, 1867 [1867b]: 34. New
name for Turbonilla graciUiyna Gabb, 1865:186, non
Chemnitzia gracillima Carpenter, 1857:431.
hai'pa. Tomatina - Cooper, 1870 [1870tl: 56, ex Dall MS
]nomen nudum]. Later validated by Dall, 1871:136-137;
160: pit. 15, fig. 11.
Leptothyra Cooper, 1867 [1867b]: 25. Type Species - "L.
sanguinea Cpr.," = Turbo sanguinewi Linnaeus, 1758:
763 (subsequent designation herein).
Remarks - A synonym of Homalapoma Carpenter,
1864b:537, 588, 627, 652, which has the same type species.
Previous workers have evidently missed Cooper's validation
of Leptothyra. dating it instead from Dall, 1871:130. It thus
becomes a senior homonym of Leptothyra Pease, 1869:70,
and if workers wish to save this name, a petiton would have
to be filed with the International Commission on Zoological
Nomenclature.
muricata, Ocinehra interfossa "var." - Cooper, 1870
[1870f]: 69, ex Carpenter MS ]nomi-u riuduin]. Not sub-
sequently validated.
paueieostata. Leptothyra - Cooper, 1867 [1867b]: 25, ex
Dall MS [nomen nudum]. Later validated by Dall, 1871:
131; 160; pit. 15, fig. 10.
sitkensis, Odostomia - Cooper, 1894 [1894b]: 100th sheet,
ex Dall MS [nomen nudum]. Not subsequently validated.
steamsiana. La.mel.la.rin - Cooper, 1870 [1870f]: 67, ex
Dall MS [nomen nudum]. Later validated by Dall, 1871:
122; 160; pit. 15, fig. 6, but as L. utearnsii.
Class Polyplacophora
fimbriatus, Callochilun - Cooper, 1867 [lS67b]: 23, ex.
Carpenter MS [ncmwn nudum]. Later validated by Keep,
1887:112, as Callistochiton fimbriatus.
latior. Planphorella - Cooper, 1894 [1894b]: 113th sheet,
ex Carpenter MS [nomen nudum]. Not subsequently
validated.
LITERATURE CITED
Carpenter, Philip Pearsall. 1857. Catalogue of the collection
of Mazatlan shells, in the British Museum: collected by
Frederick Reigen . . . London (British Museum) i-iv + ix-
xvi 4- 552 pp. (1 Aug. 1857) [Warrington ed., publ.
simultaneously] [reprinted, Paleo. Resh. Inst., 1967].
1864a. Diagnoses of new forms of mollusks col-
lected at Cape St. Lucas by Mr. Xantus. Ann. Mag. Natur.
Hist. (3) 13(76):31 1-315 (April); (78):474-479 (June);
14(79):4.5-49 (.July) [reprinted in Carpenter, 1872:
207-221].
1864b. Supplementary report on the present
state of our knowledge with regard to the Mollusca of the
west coast of North America. Brit. Assn. .Adv. Sci.. Rept.
33[for 1863]:517-686 (post-1 Aug. 1864) [reprinted in
Carpenter, 1872:1-172].
1872. The mollusks of western North America.
Embracing the second report made to the British Asso-
ciation on this subject, with other papers: reprinted by
permission, with a general index. Smithsonian Inst.
Misc. Colin. 10(252):xii + 325 + 13-121 pp. (Dec. 1872).
Coan, Eugene V. 1982. James Graham Cooper; pioneer
western naturalist. Moscow, Idaho (Univ. Press of Idaho)
255 pp.; 31 figs. (22 Feb. 1982).
Cooper, James Graham. 1867 [1867b in Coan, 1982]. Geo-
graphical catalogue of the Mollusca found west of the
Rocky Mountains, between latitudes 33° and 49° north.
San Francisco, Calif. (Geol. Survey of Calif.) 40 pp. (post-
April 1867).
1870 [1870f in Coan, 1982]. Notes on the Mol-
lusca of Monterey, California. Amer. Journ. Conch. 6(1):
42-70 (7 July 1870).
1894 [1894b in Coan, 1982]. Catalogue of west
North American and many foreign shells, with their geo-
graphical ranges. For labels, exchange, and check lists.
With a supplement. Sacramento, Calif. (Calif. State
Mining Bureau) 181 unnumbered pages grouped in stapled
sections [see Coan, 1982, for details], main body: Title
page + Preface -i- 16(1 pp.; Siippl.: Title page + 13 pp.;
Add. & Corr.: 5 pp. (April 1894).
Dali, William Healey. 1871. Descriptions of sixty new forms
of mollusks from the west coast of North America and
32 THE NAUTILllS
January 31, 1986
Vol. ]()0(1)
the North Pacific Ocean, with notes on others already
described. Amer. Journ. Conch. 7(2):9,3-160; pits. 13-16
(2 Nov. 1871).
1915. A review of some bivalve shells of the
group Anatinacea from the west coast of America. United
States Nation. Mus., Proc. 49(21 16):441-4.56 (27 Nov.
1915).
1919. Descriptions of new species of Mollusca
from the North Pacific Ocean in the collection of the
United States National Museum. United States Nation.
Mus., Proc. 56(2295):293-371 (30 Aug. 1919).
Gabb, William More. 1865. Descriptions of new species of
marine shells from the coast of California. Calif. Acad.
Sci., Proc. (1) 3(3):182-190 (.Ian. 186.'3).
Keep, .Josiah. 1887. West coast shells. A familiar descrip-
tion of the marine, fresh water, and land mollusks of the
United States, found west of the Rocky Mountains. San
Francisco (Bancroft Bros) 230 pp.; 182 figs.; frontis.
(post-July 1887).
Linnaeus, Carolus. 1758. Systema naturae per regna tria
naturae . . . editio decima, reformata 1 [Regnum animale],
Stockholm (Laurentii Salvii). 824 + iii pp.
Pease, William Harper. 1869. Descriptions of new species of
marine gasteropodae inhabiting Polynesia. Amer. J.
Conch. 5(2):64-79 (7 Oct. 1869).
Treitschke, Friedrich. 1825-1826. Die Schmetterlinge von
Europa 5. Leipzig (G. Fleischer) [pts. 1, 2 - 1825; pt. 3 -
1826).
NOTES ON THE HABITS AND ANATOMY OF THE INTRODUCED LAND
SNAILS, RUMINA AND LAMELLAXIS (SUBULINIDAE)
Dee S. Dundee^
Department of Biological Sciences
University of New Orleans
New Orleans, LA 70148
ABSTRACT
Marking experiments showed that Rumina decollata moved no more than 25
inches from points of release in a six-month period, demon.'it rating, as with most
introduced forms, that passive distribution prevails. Egg-to-egg span was slightly
over a year in the lab. While normally considered carnivorous, R. decollata ivill
feed on a variety of vegetation, and were routinely fed lettuce. Average growth is
l.J,6 mm, in width/ week and average whorl addition is 1.18 whorls/week. At 10 mm
high, the snails lose the upper 3. 0-3.. 5 whorls and fill in the top with a .'<eptum. An
individual snail may deposit 30-50 ova over a period, of several days on more than
one occasion from February to June in this area. They are deposited in shallow
depressions, and soil particles adhere to them, thus rendering them in-
conspicuous.
Notes on the anatomy and a brief histological statement of the digestive,
nervous, and reproductive systems o/Lamellaxis gracilis are given.
Since the publication (Dundee, 1970) of a
study of four introduced mollusks, further infor-
mation has been gathered about the two species:
Rumina decollata (Linnaeus, 1758) and Laniel-
laxis gracilis (Hutton, 1834). The information is
presented here as follows: (a) observations on
Rumina decollata: movement, reproduction,
growth and decollation, longevity (b) notes on
the anatomy-histology of Lamellaxis gracilis.
'Published posthumously. Dr.
Article proofed by the editor.
Dundee died May 7, 1985.
Observations on Rumina decollata
(Linnaeus, 1758)
Movements. Six marking experiments, iden-
tical to those described for Bradybaena simi-
lar is and Lamellaxis gracilis (see Dundee,
1970), were done in Greenwood Cemetery in
New Orleans. The maximum movement demon-
strated in any of the experiments was 25 inches
from the point of release over a six month
period. This seems to verify the idea that in-
troduced mollusks do not disperse through their
own power but, rather, are distributed through
Vol. 100(1)
January 31, 1986
THE NAUTILUS 33
passive means.
Reproduction. Despite Sealander's (1974)
statement concerning self-fertilization being ". . .
the major mode of reproduction . . ." in Rum inn
decollata. Batts (1957) reported, and I have
observed, regular matings between individual
snails thus suggesting that cross-fertilization is
the prevailing method in the species. Sealander
(1974), later in the paper, states that ". . . we
cannot unquivocally conclude that reproduction
in the singles involved self-fertilization rather
than parthenogenesis."
Ova were seen in both in the field and in the
lab. Rascop (1960) reported one snail producing
55-1- ova over a period of 3-5 days. In my lab
colony, the members of which began reproduc-
ing after reaching about ten months of age, the
average number of eggs/snail/deposition period
was 32. In the field, clusters of 15-41 eggs were
observed at various times. Sealander (1974), on
the other hand, reported 105 snails laying 6822
eggs or, when calculated, 64/eggs/snail average
which is considerably higher than these aver-
ages. It appears that, when one considers
Rascop (1960), Batts (1957), Sealander (1974),
and this present work, that Rumina decollata
may produce anywhere from 7-64 eggs at one
deposition period and then repeat the process
several times over a period of a few weeks.
The ova are deposited singly, but close enough
together so that they form clusters. They are
placed in shallow depressions in the soil. Deposi-
tion occurs from February to June in this Gulf
Coast area. A non-productive period then oc-
curs, followed by more egg deposition from
September to November.
Average incubation time was ten days at an
ambient temperature range of 21-27°C in the
lab. Batts (1957) reported an average time of
28.5 days but recorded no temperatures. She
also reported one incubation time of 9 days.
Sealander (1974) reported the incubation period
under laboratory conditions to be about 30 days.
He did not describe lab conditions.
Growth and decollation. Nineteen lab juve-
niles were observed for slightly over a year. The
snails, being herbivores as well as predatory car-
nivores, were given lettuce and other local snails
as food. The graph (Fig. 1) in showing constant
growth, demonstrates indirectly that this is an
adequate diet to support them since they grow
to maximum size on it.
Average growth in height in the lab at 21-
27°C is 1.46 mm/week and average whorl addi-
tion is 1.18 whorls/week. Those figures remain
valid until the snails reach 10 mm in length. At
that 10-mm point the upper 3.0-3.5 whorls are
lost and the snail is said to be "decollate". If one
I
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WHO R L S
FIG. 1. Rumina ikcollnta. This graph shows in terms of
height and number of whorls. At the 10 mm high point, the
snails become decollated thus having fewer whorls but con-
tinuing growth in height. Open circles represent non-
decollate individuals; solid dots represent decollate ones.
34 THE NAUTILUS
January 31, 1986
Vol. 100(1)
examines a 9-mm-long, non-decollate specimen
(Fig. 2), one notices a peculiar-appearing apex
area. The first 3.0-3.5 whorls have a smooth,
glassy appearance, whereas the remaining
whorls have some striations. The second major
whorl below the protoconch is inflated thus giv-
ing the top of the shell a ))uffy appearance. The
shell decollates just l)eneath the whorl below the
inflated one. I have been unable to observe how
the breakage occurs although it has been re-
ported that the snail bangs its upper whorls
violently against a hard object to get rid of them
(Cooke, 189,5). Batts (1957) reported observing
them striking the shell against rocks or the
aquarium wall to aid in decollation. A calcareous
septum, resembling the protoconch, is formed
as a cover for the top of the broken shell (Fig. 3).
It is easily seen in the decollate forms. If one
breaks off the top whorls of a 9.5-mm-long speci-
men, one discovers that the top 3.0-3.5 whorls
break much easier than those below and that
there is no septum present; it is apparently
secreted after decollation occurs. Figure 3 is a
view of a septum as one looks down on the top of
a decollate shell. Notice that the umbilicus is
retained.
Decollation occurs in widely separated taxa
from pulmonates to prosobranchs. It occurs in
terrestrial as well as aquatic forms (brackish
water). It seems to have evolved independently
several times. Examination of a serial section of
a 9-mm-long R. decollata reveals nothing
unusual about the internal anatomy in the area
which is destined to break off. One can only
speculate at this point on the selective advan-
tage of casting off part of the shell. Perhaps the
upper whorls serve as a storage for toxins dur-
ing early growth; perhaps decollation is a
behavorial matter related to habitat (e.g., ability
to get under shelter); perhaps it is only a non-
selective mutant. The entire matter needs fur-
ther study.
Longevity. The longest I have l)een able to
keep this species alive in the lab is just over a
year. Rascop (1960) reports a longevity record
of 12 years but does not cite a reference. That
seems a very long time considering longevities
of various other snails (Hyman, 1967). Years of
observations by the author have shown that
mollusks tend to reproduce just prior to the ex-
tinction of the colony. This colony, which was
followed from egg-to-egg, began reproducing at
ten months which was approximately two
months prior to the death of the last colony
member.
Observations on Lamellaxis gracilis
Shell. Figure 4 shows a typical adult shell.
The maximum size seen in the New Orleans area
F'UiS. Z and 3. Riiniiiid di'mUata. 2, A spi'cmifn of ;i|j|jnix-
irriatoly 9 mm showing the smooth quahly of the top three
whorls as opposed to the striations on the remaining ones. 3,
A view into the top of a large decollate specimen.
Vol. 100(1)
January 31, 1986
THE NAUTILUS
FIGS. 4-7. Lamelhxif: gracili.'i. 4, Adult shell.
5, An about-to-hatch snail dissected from its egg
case. 6, The jaw, 7, Central and lateral teeth.
was 13 mm in length, 3.5 mm in width at the
broadest point, and with 9.25 whorls. The maxi-
mum size of Lamellaxis micra (Orbigny, 1835)
which also has been introduced to this area was,
by contrast, 7.2 mm x 2.2 mm, and had 6.75
whorls. The color of L. gracilis is light tan and
all whorls except the protoconch are finely
striated. A small umltilicus is partially hidden by
a minor reflection of the lip (Fig. 4). Unhatched
ova (Fig. 5) removed from the female system
show clearly the beginnings of striation except
on the protoconch.
Jaw. This structure is found at the entrance
to the pharynx in a mid-dorsal position. As can
be seen in Figure 6, it is a single, curved device
which has coarse transverse ribbing.
Radula. The radula (Fig. 7) is relatively nar-
row with little variation among central, lateral,
and marginal teeth. The teeth are reminiscent
of marginals of Helix aspersa except the lateral
cusps are more pronounced.
Digestive system. The esophagiis, lined by
tall, ciliated columnar epithelium and underlain
by a thin circular muscle layer surrounding an
equally thin longitudinal layer. The esophagus
leaves the pharyngeal area, passes through the
nerve ring and posteriorly into the stomach;
(Fig. 9 ST). In keeping with other Stylommato-
phora, no crop was found. The stomach is lined
by tall, columnar, ciliated epithelium underlain
by a double muscle layer (longitudinal and cir-
cular) and surrounded by connective tissue. The
lining is folded in several areas. The digestive
gland (Fig. 8, D) empties into the stomach via
two ducts -one from each section of gland. A
dissection showing the two parts is very difficult
and can only be done with fresh (non-preserved)
material. Histological observations reveal two
cell types making up the digestive gland (also
called liver and hepatopancreas). A tall colum-
nar cell type which contains numerous vacuoles
is often seen with the lumen in a state of disinte-
gration implying secretion. The second type is a
low, non-ciliated triangular form. Carriker and
Bilstad (1946) reported similar cells and called
them "digestive" and "calciferous" and deter-
mined that the latter contain calcium phosphate
granules. Digestion is apparently both intra-
and extra-cellular. Sections reveal partially
digested material in the stomach lumen (Fig. 8,
ST) and also in some the cells of the digestive
gland. An intestine leaves the stomach, loops
around in the same whorl as the stomach,
descends to the right dorso-lateral of the head-
36 THE NAUTILUS
January 31, 1986
Vol. 100(1)
FIG. 8. Lamt'lliiji.^ ^innms. Parasagittal section of a
young snail. D = digestive gland; ST= stomach; I = intestine;
A = albumen gland.
foot where the anus is located. The intestine
(Fig. 8, I) is lined by tall, ciliated columnar
epithelium containing mucous cells and under-
lain by an inner longitudinal and an outer cir-
cular muscle layer.
Nervous system. The ganglia form a ring
around the anterior portion of the digestive
tract just posterior to the pharynx. This is the
result of detorsion wherein the parietal (in-
testinal) and visceral ganglia migrate forward
near the pleural ganglia. In Lamellaxis the end
result is two cerebral ganglia on the dorsal of
the ring and two pleurals, two parietals, and a
visceral (two fused ganglia) forming the ventral
portion of the ring and innervating the entire
visceral mass. The total nervous system was not
traced.
A pair of eyes, located on the dorsal tips of the
posterior tentacles, are typical pulmonate vesi-
cular types (Hyman, 1967, p. 584). The stato-
cysts, located adjacent to the pedal ganglia in
the foot, are small spherical vesicles each con-
taining calcareous granules. Each is covered by
a layer of connective tissue and lined internally
by a squamous-type epithelium with a layer of
cilia equally spaced around the inner periphery.
Excretory system. A single nephridium is
located near the dorso-posterior of the pulmon-
ary cavity. If one holds the snail so that the
aperture is facing him, the reno-pericardial
mass is on the extreme lower right of the whorl
above the aperture. The pericardial cavity has a
duct from it into the sac-like nephridium. That
nephridium, in most Pulmonates, opens into the
|.)ulmonary cavity directly via a slit or a short
ureter. I could not determine which is present in
this snail either by dissection or sections.
Reproductive. System. Lamellaxis is herma-
phroditic. The ovotestis, a grapelike cluster
embedded in the digestive gland proximal to the
columella, contains both oocytes near the peri-
phery of each follicle and spermatocytes and
sperm more centrally located near the duct of
each. A coiled hermaphroditic duct, lined by low
ciliated cuboidal epithelium, drains both the
ovary and testis. At the lower end of that duct a
small saclike structure, the seminal vesicle, ap-
pears to branch off and serves as a sperm stor-
age area. It is seen full of sperm during the
breeding season. Near that point, the male and
female systems part company with each system
continuing downward, closely applied to and
paralleling each other (spermoviduct of some
authors) through the whorls towards the
anterior end.
The male system consists of a sperm duct (vas
deferens) with a ciliated cuboidal lining. It
receives a prostatic secretion via a small connec-
tion between the prostate and vas deferens. The
prostate consists of cuboidal cells around an ir-
regular lumen. The cells closest to the lumen
disintegrate as a result of secretion. Nuclei are
basal. The vas deferens continues downward
and enters the verge. Just prior to that entry
the duct liecomes lined by tall, ciliated glandular
epithelium. The system empties on the right side
of the head near the base of the right tentacle.
The verge is simply a long attenuated tubule
with no secondary structures on it. At the point
where the systems become separate the oviduct
appears to enter a large albumen gland but,
actually, the gland is large enough that it has
the oviduct "embedded in" it (Fig. 9, A). The
allmmen gland has a varied histological struc-
ture ranging from cuboidal to low, ciliated,
Vol. 1(H)(1)
January 31, 1986
THE NAUTILUS 37
epithelial cells. This gland, in section, always ap-
pears striated and somewhat "crumbled". The
lumen ends of the cells appear to disintegrate as
secretions are formed.
Just ventral to this albumen gland, at the
separation of the male-female systems is an area
where fertilization occurs (fertilization pouch or
carrefour in other pulmonates: e.g., (Petrellis
and Dundee, 1969). A distinct pouch could not
be located in L. gracilis. Only a slightly swollen
area in the hermaphroditic duct exists. It is dif-
ferent histologically from the initial part of the
duct in that the epithelium is ciliated columnar
in contrast to low, non-ciliated cuboidal in initial
portion of the duct. The change in histological
structure indicates that the area is the equiva-
lent of the fertilization pouch and is doubtlessly
the site of fertilization.
Fertilized eggs receive their albumen coat as
they pass by the albumen gland. As they con-
tinue anteriorly downward, the shell is added by
the mucus gland (also called capsule gland)
which is a continuation of the large glandular
mass. The albumen and mucus glands can be dis-
tinguished microscopically by change from whit-
ish, coarse appearance (albumen) to a smooth
yellowish one with the entire mass convoluted
(mucus). Microscopically the mucus gland dif-
fers from the albumen gland described above by
being a highly glandular mass lined by cuboidal
cells which, in many cases, are secreting as
evidenced by the disintegrated inner cell mass.
Non-secretory cells are ciliated, and cell boun-
daries are indistinct.
Often as many as 6-8 large ova can be seen
lined up in the oviduct in the body whorl and the
one immediately above it. Just at the point
where ova emerge from near the mucus gland,
the vagina receives a duct from the spermatheca
(also called seminal receptacle or bursa), a sac
which stores sperm from copulation. Histologi-
cally the spermatheca is composed of non-
ciliated, tall columnar epithelium encapsulated
in a muscle-connective tissue layer. The vagina
is a muscular tubule lined by ciliated epithelium.
It ends at the gonopore which is found in the
right dorso-lateral area of the head.
LITERATURE CITED
Batts, Jeanne H. 1957. Anatomy and life cycle of the .'^nail
Rumina decollata. Southwest Nat. 2:74-82.
Biswas, S. K.. R. Rahman and T. R. Mitra. 1976. Observa-
tions on the breeding habits of Opeas gracile (Hutton)
(Gastropoda: SubuMnidae). .Jour. Conch. 29:69-70.
Carriker, Melbourne and N. M, Bilstad. 1946. Histology of
the ahmentary system of the snail, Lymnnen stagnalis
(ippressa. Trans. Amer. Micr. Soc. 64:250-275.
Cooke, A. H. 1895. In Cambridge Natural History Vol. HI
(Molluscs and Brachiopods). Macmiilan & Co. (Reprint
edition: 1-ix + 535; 334 figs.; 1 map. Wesley, Ltd.,
England, 1959).
Dundee, Dee S. 1970. Intro<luced Gulf Coast molluscs.
Tulane Studies in Zool. and Bot. 1G(3):101-115.
Dundee, Dee S. and Roy J. Baerwald. 1983. Observations on
a micropredator, Gulella bicolor (Hutton), (Gastropoda:
Pulnionata: Streptaxidae). The Nautilus 98(2):63-68.
Hyman, Libbie H. 1967. The Inverteljrata: Vol. VI Mollusca
'l: i-vii + 1-792; 249 figs.; McGraw Hill Book Co.
Petrellis, Louisa S. and Dee S. Dundee. 1969. Veronicella
ameghini (Gastropoda: Reproductive, Digestive, Nervous
system). Trans. Amer. Micr. Soc. 88(4):547-558.
Rascop. Ann M. 1960. The biology of Rumuin decollata.
Unpub. M.A. Thesis. Univ. Ariz.
Sealander, R. K., D. W. Kaufman and S. Ralin. 1974. Self-
fertilization in the terrestrial snail Rumina decollata.
Veliijer 16(3):265-270.
New Awards
The Division of Mollusks, Department of
Invertebrate Zoology, National Museum of
Natural History, Smithsonian Institution
announces the availability of two fellowships to
be awarded to graduate students of systematic
malacology.
1. Rosewater Fellow Award (up to $500)
2. Smithsonian - Conchologists of America
Fellow Award (up to $1,000)
These awards are to help support students for
short term research visits to the collections and
libraries of the Division of Mollusks, National
Museum of Natural History and are to be used
for systematic studies of Mollusca. Funds can
help cover travel, subsistence, and research
costs [xerox, postage, etc.]. Interested students
should submit a 1-page proposal, a budget with
indication of matching funding, if available, and
a supporting letter from their faculty advisors.
Deadline for applications is March 1, 1986.
Awards will be announced on April 1, 1986.
38 THE NAUTILUS
January 31, 1986
Vol. 11)0(1)
NOTES
NOTE ON CRYPTONATICA DALL, 1892
(GASTROPODA: NATICIDAE)
Richard E. Petit
806 St. Charles Rd.
North Myrtle Beach, SC 29582
The naticid subgenus Cryptonatica was pro-
posed by Dall (1892:362) with no type designa-
tion. Dall's first mention of Cryptonatica {p. 362)
lists the species Natica clausa Broderip &
Sowerby, A'^. russa Gould and A'^. pusilla Say as
being included. A few pages later (p. 366) the
new species Nafica (Cryptonatica) floridana is
described. As pages 362-366 were published at
the same time, all four of these taxa are original-
ly included species and are available for designa-
tion as type-species of Cryptonatica.
Cossmann (1896:238) in a review of Dall's
1892 publication designated A'^. (C.) floridana
Dall as the type of Cryptonatica, an action
overlooked by all subsequent authors, including
Cossmann himself. Dall (1909:85) designated A^.
claMsa Broderip & Sowerby as type, and this
species has been accepted as type (although with
differing citations for the designation) by all
subsequent authors. Among those citing A^.
claitsa as type of Cryptonatica are Cossmann
(1925:120), Woodring (1928:384), Boss,
Rosewater & Ruhoff (1968:95), and Marincovich
(1977:409).
Natica. clausa. is a cold-water Recent species
and A^. floridana is from the Florida Oligocene.
It is not the purpose of this paper to investigate
or discuss the probable relationship of these
species or the ramifications possible as a result
of Cossmann's type-designation, but to call to
the attention of naticid systematists it's ex-
istence so that appropriate action may be taken.
Cossman often made type designations in his
reviews which appeared in various publications
from 1888 to 1924. A listing of these designa-
tions is now in preparation and will be published
in the future.
LITERATURE CITED
Bo.ss, K. .1., ,1. Rosewater and F. A. Ruhoff. 1968. The
Zoolo)rical Taxa of William Healey Dall. U.S.N.M. Bull.
287:1-427.
Cossmann, M. 189(). Revue de Paleoconcholofjie. La Feuillc
des Jeunes Naturalistes 26(:3I2):2:i0-24().
1925. Naticidae. Essais de Paleoconchologie
Comparee 13:97-150.
Dall, W. H. 1892. Contributions to the Tertiary Fauna of
Florida ... Wagner Free Inst. Sci. 3(2):201-473, pis. 13-22.
1909. The Miocene of Astoria and Coos Bay,
Oregon. U.S. Geol. Surv.. Prof. Paper 59:1-278, pis. 1-23.
Marincovich, L., Jr. 1977. Cenozoic Naticidae (Mollusca:
Gastropoda) of the Northeastern Pacific. Bull. .Amer.
Paleont. 70(294):16.5-494, pis. 17-42.
Woodring, W. P. 1928. Miocene Mollusks from Bowden,
Jamaica. Pt. II. Gastropods and Discussion of Results.
Carnegie Inst. Wash. Publ. 385. 564 pp., 40 pis.
NATICA (GLYPHEPITHEMA) BAYERL
NEW NAME
Harald A. Rehder
National Museum of Natural History
\ Smithsonian Institution
Washington, D.C. 20560
Richard E. Petit has called my attention to the
fact that the species in the Naticidae that I
described as Glyphcpithema floridana in 1943
(Proc. U.S. National Museum: 93(3161):196-197,
pi. 19, figs. 19-21) is preoccupied by Natica
(Cryptonatica) Jloridana Dall, 1892, described
from the Oligocene of the Tampa formation
(Trans. Wagner Free Inst. Sci. Philadelphia
3(2):366, pi. 17, fig. 5). The taxon Glyphepit he-
ma. Rehder, 1943 (op. cit., p. 196), originally
proposed by me as a genus, is now quite general-
ly cited as a subgenus of Natica. and therefore
the species name floridana Rehder needs to be
replaced.
I propose to name this species Natica (Gly-
phepitheyna) bayeri Rehder dedicating it to my
longtime associate and friend, F. M. "Ted"
Bayer, who collected the holotype in Lake
Worth, Florida. The species is found from south-
eastern Florida to Panama and northeastern
Brasil (Abbott, American Seashells, ed. 2, p.
159, 1974).
DEATHS
A. Myra Keen - 1905 - 1986
One of the great giants of American malacology, Angeline
Myra Keen, died on January 4, 1986, at the age of 80 in
California. Dr. Keen was one of the leading forces in the
development of students in malacology at Stanford Univer-
sity, and well-known not only for her excellent taxonomic
work hut also for her major contribution of popular books
that aided legions of appreciative private shell collectors.
She assisted and gave advice to many amateurs who wished
to publish on mollusks.
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APRIL 30, 1986
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Woods Hole, Mass.
THE
NAUTILUS
Volume 100, number 2 - April 30, 1986
ISSN 0028-1344
CONTENTS
Thomas R. Waller
A New Genus and Species of Scallop (Bivalvia: Pectinidae) from off Somalia,
and the Definition of a New Tribe Decatopectinini 39
Hans Bertsch and Antonio Mozqueira Osuna
A New Species of Triton in (Nudibranchia) from Southern California and Baja California 46
Arthur H. Clarke
Unionidae of the Upper Connecticut River, a Vanishing Resource 49
Jose Gomez, Mercedes Vargas and Emile A. Malek
Morphological Anomalies in the Shell of P"ield-CiilleetedS('(W(/)/;a/(/n'(( glabratn (Say, 1818). . . .53
Eva Pip
The Ecology of Freshwater Gastropods in the Central Canadian Region 56
Jose Gomez, Mercedes Vargas and Emile A. Malek
Pseudosuccinea columella (Lymnaeidae) in the Dominican Republic and
Transmission of Fascioliasis in the Caribbean Region 66
David Nicol
Some Aspects of the Evolution of the Rudist Pelecypods 69
Mark E. Gordon
A New Sitmatogyrus from the Southwestern Ozarks with a Brief Review
of the Hydrobiidae from the Interior Highlands (Gastropoda: Prosobranchia) 71
Anthony D'Attilio and Barbara W. Myers
Favartia brericida (Sowerby, 1834) and Two New Species of Favurtia
from the Western Pacific (Gastropoda: Muricidae) 78
New Mollusk Journals 55 Meeting News 68
SEASHELL
TREASURES
or THE CARIBBEAn
text and photographs
LESLEY SUTTY
(under the editorship of R. Tucker Abbott)
Follow the personal adventures of a marine biolojjist as she hunts throu^^hout the West Indies
for elusive and rare seashells. An active naturalist and archaeologist. Miss Suttv has spent years
in photoj^raphing and observinjj marine life and studying the uses of shells by the ancient Carib
Indians. Under the editorial guidance of Dr. Abbott this book serves as an accurate guide to the
most unusual shell treasures of the Caribbean.
New Discoveries
Not seen since first discovered 35 years iigo. Straus's
Murex (Hexaplex strausi Verrill, 1950) was found alive
in 21 feet of water in Martinique. Lesley re-discovered
Lamarck's long-lost Picrynoius plnllopwnis as early as
1469. and she is the first to record a case of a human
being slung by a West Indian poisonous cone shell.
Deep Dive Photos
For the first time, a living specimen ot the rare
Surinam Cowrie is photographed during a night scuba
dive. See an eyeball-to-eyeball photo ot the queer
Umbrella Shell (Umhracuhtm). and thrill to the color
shots of intricate niulihranch sea slims.
A UNIQUE SHELL BOOK!
This unusual book is a blend of beauty,
adventure and science:
/. 11)0 rare spccu-s illuslnilVit in i^oiin'ous color.
2. Details of where llwv live and how lo find them.
.?. SeieiUijie and eoinnion names, each nitli author and dale.
4. (ieoi;ra/)hieal oceiirreme. depth and relative abiindancv.
5. Colleclini; experiences ihroii^lunii the .\nlilles.
6, I'aeked with /icir hiolofiieal ohser\ati(nis.
May 1986. cloth
NATURAL HISTOKY/COLLCCTinQ 138 color plates
Bibliography Index 7'/2 x 9%" 128 pages
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TREASURES OF THE CARHJBEAN.
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Vol. 100(2)
A()ril 30, 1986
THE NAUTILUS 39
A NEW GENUS AND SPECIES OF SCALLOP
(BIVALVIA: PECTINIDAE) FROM OFF SOMALIA,
AND THE DEFINITION OF A NEW TRIBE DECATOPECTININI
Thomas R. Waller
Dt'pai'ttiifiit (if Paleobiology
U. S. National Museum of Natural History
Smithsonian Institution
Washing-ton, DC 205(i0
ABSTRACT
Somalipecten Waller, new genus, is one often extant pectinid genera that are
placed in the new tribe Decatopectinini, which is characterized by low early beak
inflation, very closely spaced commarginal lamellae, and very weak or absent
resilial hinge teeth. The type species, Somalipecten cranmerorum, new species,
from offSom.alia in 1.50-300 m. is the sole survivor of a group of congeneric species
that lived in the Neogene and Quaternary if the Red Sea and we.^terti Indian
Ocean regions.
Introduction
Many new species of shelled moilusks are still
being discovered in the world's oceans, but it is
remarkable when a new species turns out to be
large in size, exquisitely beautiful in color and
form, and also abundant at its type locality in a
region thought to have a well-known moUuscan
fauna. In this report I describe a new scallop,
Somalipecten cranmerorum. new genus and
species, taken by Taiwanese trawlers working
new fishing grounds off Somalia. This new pec-
tinid genus, which has an extensive fossil record
in Neogene and Quaternary strata adjacent to
the Red Sea and western Indian Ocean, is one of
ten extant genera that comprise a yiew tribe.
Decatopectinini.
The system of measurement used here follows
that in Waller (1969, 1972), in which shell height
is measured as the perpendicular distance be-
tween the active outer ligament or hingeline and
a parallel line drawn through the most ventral
point on the ventral margin. References to
numbers of teeth in the ctenolium refer only to
the active ctenolium (Waller, 1984), not the in-
active ctenolium partially obscured by the
growth of the anterior auricle. The umbonal
angle is the angle between lines diverging from
the origin of growth and passing through the
estimated points of union between the free
margins of the auricles and the disk flanks.
Observation of microsculpture was by means of
a Wild M-.5 binocular microscope at magnifica-
tions not exceeding x 50. Measurement
employed an ocular micrometer as well as a
goniometer eyepiece.
The term antimarginal is introduced with
reference to microsculpture that maintains a
nearly perpendicular relationship to the shell
margin, exemplified by the Camptonectes micro-
sculptural pattern (illustrated in Waller, 1972).
In contrast, sculptural features such as plicae,
which are described as radial, are perpendicular
to the shell margins only in the midventral
region and may be nearly parallel to margins in
the region of the disk flanks. These terms com-
plement the term commarginal, which has come
into broad usage for features that are parallel to
shell margins. I also propose new terms found to
be useful for the description of hinge teeth in the
Pectinacea. In the right valve, resilial teeth
originate near the origin of growth of the shell
and approximately parallel the anterior and
posterior sides of the resilium, at least in early
ontogeny. One such tooth borders each side of
the resilium, as in Chlamys islandica (Miiller,
1776). Dorsal teeth lie immediately ventral to
the outer ligament, one such tooth bordering the
outer ligament on each side of the hinge, and
may originate at some distance from the origin
of growth (arrows in Fig. 13). Intermediate teeth
lie between resilial and dorsal teeth, are com-
monly differentially developed on the anterior
40 THE NAUTILUS
April :^0, 1986
Vol. 100(2)
and posterior sides of the hinge, and may be
multiple, as in Decatopecten and Pecten.
The anatomy of Snmaiipecfev cranrnerorum-
cannot Ix' described at {)resent, because no soft
parts were available to me.
Systematics
C/a.s.s Bivalvia Linnaeus, 1758
Subclass Pteriomorphia Beurlen, 1944
[e)n<')id.. Boss, 1982]
Superorder Eupteriomorphia Boss, 1982
Order Ostreoida Waller, 1978
Suborder Pectinina Waller, 1978
Superfamily Pectinacea Rafinesque, 1815
[emend. . Waller, 1978]
Family Pectinidae Rafinesque, 1815
[emend., Waller, 1978]
Subfamily Pectininae Rafinesque, 1815
Tribe Decatopectinini, new tribe
Diagnosis: Pectinidae having very closely
spaced commarginal lamellae at least in early
ontogeny and commonly throughout life, the
spacing commonly ranging from about 30 to 70
lamellae per two-millimeter distance along a
radius in center of disk at height of 10 mm; infla-
tion of left beak very low, only very slightly ex-
ceeding that of right beak, the left beak extend-
ing only very slightly dorsal to hingeline; anti-
marginal microsculpture very fine and
restricted to early ontogeny of disk to a distal
limit slightly beyond origins of radial plicae,
absent from disk flanks and auricles; dentition
dominated by dorsal and/or intermediate teeth,
the latter sometimes multiple or sometimes
absent; resilial teeth low or absent.
Type Germs: Decatopecten Ruppel in Sowerl)v,
1839.
Taxonomic Composition-The new tribe con-
tains the following extant genera, listed with
their type species, geographic region, and some
common synonyms:
Anguipecten Lall, Bartsch, and Rehder, 193S,
type spac'w^ Anguipecten g7-egoryi Dall, Bartsch,
and Rehder, 1938 [junior synonym of Perl en
Uintherti Souverbie //( Sourverbie and Mon-
trouzier, 1874], tropical Indo-Pacific.
Annachlanii/s Iredale. 1939, type species
Pecten Icopardus Reeve, 1853 [junior synonym
o\ Pecten flabellat us Lamarck, 1819|. tropical
western Pacific and eastern Indian Oceans.
Bractechlamys Iredale, 1939, type species
Bractechkimys evecta Iredale, 1939 [junior
synonym of Pecten vexillum Reeve, 1853],
tropical Indo-Pacific and Western Atlantic.
Decatopecten Ruppel in Sowerby, 1839
[senior sync^nym of Comptopallium Iredale,
1939], type species Ostrea plica Linnaeus, 1758,
tropical Indo-Pacific.
Excellichlamys Iredale, 1939, type species
Pecten spectabilis Reeve, 1853, tropical Indo-
Pacific.
Flexopecten Sacco, 1897 [senior synonym of
Glabropecten Sacco, 1897, Lissopecten Verrill,
1897, and Proteopecten Monterosato, 1899],
type species Ostrea jlexuosa Poll, 1795, Mediter-
ranean and adjacent eastern Atlantic.
Gloripallium Iredale, 1939, type species
Ostrea jialUitin Linnaeus, 1758, tropical Indo-
Pacific.
Juxtamusiiim Iredale, 1939, type species
Juxtatnusiutn. ublectatum Iredale, 1939 [junior
synonym of Pecten (Chlamys) coudeini Bavay,
1902], tropical western Pacific and Indian
Oceans.
Mirapecten Dall, Bartsch, and Rehder, 1938,
type species Mirapecten thaanumi Dall,
Bartsch, and Rehder, 1938 [junior synonym of
Pecten mirificus Reeve, 1853], tropical Indo-
Pacific.
Somalipecten Waller, new geyius. type species
Sonialipeeten erannieroriun Waller, new species
described herein, tropical western Indian
Ocean.
St rat Igraphic Range: Paleocene to present.
Discussion: In view of the common assump-
tion that commarginal increments in many
bivalves are periodic, indicative of growth rate,
and hence subject to environmental modifica-
tion, it would seem inapjiropriate to use com-
marginal spacing as one of the prime morpho-
logical differentia for a tribe. However,
evidence is accumulating showing that growth
increments are not always periodic and may
occur in ways that are taxonomically specific
and hence genetically determined (Jones, 1981;
Ohno, 1985). Recently, Helm and Malouf (1983)
suggested that there may be a minimal required
distance between successive commarginal
ridges in the Atlantic Bay Scallop. .Argopecten
irradians (Lamarck, 1819), and that this re-
Vol. 100(2)
Ai)ril 30, 1986
THE NAUTILUS 41
(luirenieiit may oN'erride any peiioiJicity when
the rate of shell growth is low. (iruffydd (1981)
showed that in Peden nidxhitiis (Linnaeus,
17.'i8) faster growth is achieved by increasing
both the width of growth increments and the
number of ridges formed per unit of time.
Whatever the cause of j)rojecting commarginal
lamellae in the Pectinidae, it is clear that these
features are more closely spaced in members of
the trilie Decatopectinini than in other scallops
at a comparable shell size at least during early
ontogeny. With few exceptions, genera outside
the Decatopectinini have fewer than 25 com-
marginal lamellae per two-millimeter space at a
height of 10 mm, and many of these have as few
as 5 to 1.5.
As can be seen from the above list of geo-
graphic ranges of genera, the Decato{:)ectinini
are largely Indo-Pacific at present, and my own
unpublished data on fossil distriliutions in-
dicates that the trilie has been primarily Indo-
Pacific throughout its geologic history. The two
exceptional genera which also occur in the
Atlantic, Bracfixhiamifs and Flexopecten. both
appear to have dispersed into the Atlantic from
the Indo-Pacific, but from opposite directions.
The relationship of Nodiperten Dall, 1898, and
Lyropertev Conrad, 1862, to the Decatopectinini
is close, but both of these genera have more-
widely-spaced commarginal lamellae, stronger
intermediate teeth, and coarser umbonal micro-
sculpture. A full account of the morphological
differences that distinguish genera in the
Decatopectinini, as well as a discussion of fossil
history, zoogeography, and relationships to
other suprageneric units within the Pectinidae,
is in preparation.
Somalipecten Waller, new genus
Type Species: Somalipecten cranynerormn
Waller, new species, from off Somalia, depth
150 to 300 m.
Diagnosis: Plicate Decatopectinini having
both valves convex, byssal notch only moderate-
ly deep, left umbo only slightly convex or flat-
tened, and disk with uneven curvature, incipient
ledging, or widely spaced nodes at least in early
ontogeny; secondary radial costae present dis-
tally; auricular costae on right posterior auricle
weakly developed and few in number or absent;
enlarged scales, if present, limited to left valve;
dentition dominated l.)y dorsal teeth, intermedi-
ate teeth weak, resilial teeth commonly absent.
TaxoYiowic Content: The new genus includes a
number of fossil species from the western
Indian Ocean region described in publications by
Cox (1929) and Eames and Cox (1956): Chlamys
(Acquipecten) /(trsanensis Cox, 1929, C. (A.)
isthmica (Fuchs, 1878), C. (A.) leesi Cox, 1929,
C. (A.) lessepsi (Fuchs, 1878), C. (A.) pseudola
Eames and Cox, 1956, C. (A.) iverthi (Philippi,
1901), and C. (A.) wyllei Cox, 1929.
Sfrdtigrajihic Range: Upper Miocene to pre-
sent. All of the fossil species listed above, with
the exception of S. pseudola, are from deposits
adjacent to the Red Sea (Egypt, Sudan, Saudi
Arabia), the western Indian Ocean (Somalia,
Kenya, Tanzania, Zanzibar), and the Arabian
Sea (southeastern Saudi Arabia, Iran). Their
age was called "post-Miocene" by Cox (1929),
and some are probably as young as late Pleisto-
cene or Holocene. S. pseudola from Iran was
said by Eames and Cox (1956) to range from
Upper Miocene to Pliocene. Somalipecten cran-
merorum. new species, is the only known living
species.
Comparison: A somewhat flattened left umbo
is also present in Annachlamys, which differs
from Somalipecten in having a wider umbonal
angle, in having commarginal lamellae which
revert to a far-set condition late in ontogeny,
and in lacking nodes, enlarged scales, or exten-
sive secondary radial costae. Some members of
Bractechlamys. specifically B. langfordi (Dall,
Bartsch, and Rehder, 1938) and B. noduliferum
(Sowerby, 1842), have nodes and ledges but dif-
fer from Somalipecten in having persistent deep
byssal notches, strong intermediate teeth, and
strong costae on all auricles. Y^xi'dnt N odipecten
Dall, 1898, and fossil Lyropecten Conrad, 1862,
and Macrochlamis Sacco, 1897, differ in having
far-set commarginal lamellae and much
stronger intermediate hinge teeth. Flexopecten
of the Mediterranean and eastern Atlantic dif-
fers in hinge details, the right dorsal teeth being
much weaker or absent, and lacks nodes or
enlarged scales. Mirapecten maintains a deep
byssal notch throughout ontogeny and has
enlarged scales on at least the posterior plica of
both valves. Notochlamys Cotton, 1930, differs
from Somalipecten in having persistent
shagreen microsculpture, and Mesopeplum dif-
42 THE NAUTILUS
A()ril 30, 1986
Vol. 100(2)
fees in having far-set coinmarginal lamellae and
prominent resilial teeth.
Somalipecten cranmerorum
Waller, ncir spceivs
Figs. M.3
Diagnoda: Somalipeden having four major
pHcae on right valve and three on left, the left
valve also having a single plica of smaller ampli-
tude adjacent to each disk flank; enlarged distal-
l.y concave or enclosed scales few in number and
widely spaced, limited to tops of plicae of left
valve.
Description: Disk Outline -Moderately large,
with height commonly 40 to 70 mm and seldom
exceeding length, the ratio of height to length
commonly 0.88 to 1.01; outline acHne or slightly
prosocline, rarely slightly opisthocline, and
equilateral; anterior and posterior extremities
of disk narrowly rounded, ventral margin broad-
ly rounded; umbonal angle ranging from 93 to
104°; both valves convex, the right more so than
the left, the umbone of left valve flattened; ratio
of convexity of closed valves to height 0.22 to
0.37, averaging 0.31.
Auricle Outlines -Right anterior auricle with
byssal notch only moderately deep, bordered on
its ventral side by an active ctenolium of from 3
to 5 delicate, closely spaced teeth, which may be
obsolescent in largest specimens; other auricles
pointed, their free margins forming acute
angles with hinge line; anterior auricles ex-
ceeding posterior in length, the ratio of length
of anterior outer ligament to length of posterior
outer ligament commonly 1.04 to 1.24; ventral
migration of ligament system absent even in
largest individuals.
Exterior Shell Surface -Right disk with 4
major plicae, at least the central ones beginning
at a shell height of between 2 and 3 mm as pairs
of low rounded costae with narrow raised crests,
each pair then merging into a single broad
rounded plica at shell height of 10 to 15 mm, the
broad plica becoming flattened and bifid with
the introduction of a median groove at a shell
height of about 35 to 40 mm; anteriormost
major plica bordered anteriorly in early onto-
geny by a single costa along edge of disk flank;
posteriormost major plica bordered posteriorly
by a pair of costae in early ontogeny. Left disk
with three major plicae bordered on anterior
and posterior by a single lower plica, the broad
interspaces broken by introduction of smaller
median plicae corresponding to the median
grooves on right plicae. Secondary radial costae
beginning on tops of right plicae at shell heights
between 4 and 12 mm and across both plicae and
interspaces of both valves by a height of 40 to 55
mm. Disk flanks without radial or antimarginal
costae. Right anterior auricle commonly with 5
to 7 costae at margin; other auricles with highly
variable costation, the right posterior auricle
commonly lacking or having only a few costae.
Enlarged, distally concave scales, sometimes
closed to form hollow knobs, limited to tops of
the five major plicae of left valve, few in number
and widely spaced, commonly fewer than 5 per
plica, rarely absent or as many as 8 per plica.
One or two commarginal ledges commonly pre-
sent in distal fourth of disk. Prismatic stage of
right valve extending to shell height of 1.8 to 2.3
mm. Microsculpture on left beak and early post-
prismatic stage of right valve before start of
commarginal lamellae consisting of exceedingly
fine antimarginal striae. Commarginal lamellae
closely spaced throughout ontogeny, first ap-
pearing in interspaces of right disk at shell
heights between 4 and 6 mm.
Internal Features- Dentition with dorsal
teeth dominant, intermediate teeth very weak
or absent, resilial teeth absent. Single crus pre-
sent on inner surface of shell beneath each disk
tlank, a second crus sometimes present on ven-
tral fourth of posterior auricles; other crura or
marginal denticles generally absent on inner
surfaces of auricles. Inner surfaces of plicae
with carinate edges and commonly with numer-
ous radially elongate marginal denticles.
Ostracum inside pallial line consisting entirely
of lathic calcite with coarse irregular patches of
folia; crossed lamellar aragonite absent in
mature shells.
Color -Basal pigment red, orange-red, or
orange, either solid or broken by exceedingly
fine white mottling and/or by bold oblique bars
or chevrons of white; dark pigment commonly
present on ventral sides of enlarged scales. Pig-
ment more subdued on right valve than on left,
the bold patterns generally restricted to left
valve. Beaks commonly with fine intersecting
diagonal white lines. Interior of shell commonly
{)igmented outside pallial line and more rarely
Vol. 100(2)
April 30, 1986
THE NAUTILUS 43
FIGS. 1-9. Holotype of Somali jjecten cranmerorum Waller, new genus and species, USNM 8590.34. length .53.8 mm, from off
Somalia, 150-300 m. 1-6, Left exterior, dorsal, right exterior, anterior, left interior, and right interior views, ammonium
chloride coating. 7, Left exterior, uncoated. 8, Detail of commarginal lamellae in central interspace of right valve at heights
between 14.7 and 17.1 mm, coated with ammonium chloride. 9. Right exterior, uncoated.
44 THE NAUTILUS
April 30, 1986
Vol. 100 (2)
FI(;S. 10-13. Views of two paratypes o{ Somalipectcn cranmerorum Waller, new genus and species, coated with ammonium
chloride. 10, Right exterior of the largest paratype, USNM 859035, length 80.5 mm, from off Somalia, 150-300 m. 11, Closed
scale with artificial perforation and an open scale on a central plica of left valve of another paratype returned to Mr. Dan, width
of open scale 4.8 mm, shell height at level of open scale 57 mm. 12-13, Left exterior and right hinge area of the largest
paratype, USNM 835095, shell length 80.5 mm, hinge length 37 mm., arrows in Fig. 13 point to dorsal hinge teeth.
inside jiallial line by the same color present on
exterior.
Comparison: Somalipecten cranmerorum,
new species, differs from all of the fossil species
mentioned in the above discussion of Somali-
pecten, new genus, in having fewer major plicae.
The smallest number of plicae among the fossil
taxa occurs in Sovialipecfen wyllpi (Cox, 1929),
which has an additional pair of plicae on each
valve, stronger intermediate hinge teeth, and no
enlarged scales on the left valve. S. cranmero-
rum superficially resembles the more coarsely
plicate varieties of Flexopecten ,(//(;/>cr (Linnaeus,
1758) living in the Mediterranean, Init that
species lacks nodes and enlarged scales and dif-
fers in hinge details, as discussed above in the
comparison of genera. None of the extant or
extinct species of Nodipectcn have as closely
spaced commarginal lamellae, and they have
much more massively developed dorsal and
intermediate hinge teeth.
Ecdiogy: The habitat of the new species is
known only from the data provided by
Taiwanese fishermen, who said that the shells
were trawled off Somalia at depths of 150 to .'500
m. Because they have not divulged the exact
locality, it is not known whether the specimens
are from the Gulf of Aden or the Indian Ocean
side of Somalia. Mr. T. C. Lan of Taipei,
Taiwan, who obtained the specimens from the
Taiwanese fishermen, has provided a list of
associated species, some of which would appear
to shed light on the locality of the pectinids.
Strombu>! otdi Emerson, 1965, was originally
described from the Indian Ocean side of Somalia
in the vicinity of Obhia and Mogadiscio (Emer-
son, 1965), and recently it also has been found
off Oman in the Arabian Sea (David Hargreave,
/)cr.s-. com.. 1986). It is not known to occur in the
Red Sea or the Gulf of Aden. Cypraea hroderipi
Soweri)y, 1832, Cypraea marginalis Dillwyn,
1SI7, and Vanum Iruncafum (Sowerby, 1892)
are known mainly from the Indian Ocean and
not the Red Sea (Abbott and Dance, 1982), and
Mi))><ichlamys toicn.scndi (G. B. Sowerby III,
1.S95) is known mainly from the Arabian Sea off
Pakistan and from the Gulf of Oman. Although
these data suggest that S. cranmerorum is from
the Indian Ocean side of Somalia, the fossil
species that is morphologically the closest, S.
iryllfi (Cox, 1929), is from a raised beach on the
Red Sea coast in Sudan.
Vol. 100(2)
April 30, 1986
THE NAUTILUS 45
The epifauna of the shells ofS. cranmerorum
gives some clues to living habits. The lower
(right) valves of many of the uncleaned speci-
mens are encrusted by cheilstome bryozoans at
least in the dorsal region and in some cases ex-
tensively over the valve. This indicates that the
lower valve was not buried in fine sediment and
that the scallop must have lived attached by a
byssus above the bottom or on a hardground
bottom. The presence of calcareous algae on the
upper valve suggests that the specimens lived in
the photic zone, as does also their association
with algal grazers such as Strombus.
Thirteen of the 52 specimens of S. cranmero-
rum examined have circular corroded patches
within which a borehole occurs over the antero-
dorsal disk flank over the approximate position
of the scallop's mouth. These features are iden-
tical to the scars produced by the calyptreacean
gastropod Capulus danieli (Crosse, 1858)
described by Orr (1962; see also Matsukuma,
1978) from another Indo-Pacific member of the
Decatopectinini, Bractechlamys vexillum
(Reeve, 1853). On the basis of gut contents,
absence of damage to soft parts other than the
mantle through which the boring passes, and
evidence of repair and continued survival, Orr
concluded that the snail-scallop relationship is
one of antagonistic symbiosis, not true para-
sitism, the snail stealing food, probably in mucus
strings, from the mouth region of the scallop.
On all but one of the scarred and bored scallops,
the shell damage is on the left umbo. The fact
that gastropod was able to survive on the lower
valve is additional evidence that the scallop lives
attached above the sediment surface.
Etymology: This species is named in honor of
Roberta D. Cranmer and her late husband,
Charles E. Cranmer, of Louisville, Kentucky,
whose personal involvement and quiet philan-
thropy have greatly benefited many people and
organizations, a number of which have made
significant contributions to malacology.
Holotype: USNM 859034, a pair of matching
valves, height 50.0 mm, length 53.8 mm, con-
vexity across closed valves, 15.5 mm, collected
by Taiwanese fishermen off Somalia at a depth
between 150 and 300 m.
Material: In addition to the holotype, USNM
859034, 51 paratypes were studied, all paired
valves from the same locality at 150-300 meters
off Somalia. Twelve of these paratypes are
deposited in the U.S. National Museum of
Natural History under the catalogue numbers
859035 (the paratype illustrated herein) and
859036 (eleven unillustrated paratypes). Thirty-
one of the remaining paratypes were returned
to Mr. Donald Dan, and one paratype was sent
to each of the following eight museums:
American Museum of Natural History, New
York; Natural History Museum of Los Angeles
County, Los Angeles; British Museum (Natural
History), London; Museum National d'Histoire
Naturelle, Paris; Rijks-museum van Naturlijke
Historie, Leiden; Australian Museum, Sydney;
Western Australian Museum, Perth; and Na-
tional Science Museum. Tokyo.
Acknowledgments
The possibility that the scallop shells from off
Somalia were of a new species was first con-
sidered by Mr. Donald Dan of Maryland and Mr.
Al Demartino of Naples, Florida, who brought
specimens to my attention. I am particularly
grateful to Mr. Dan for providing a large
number of specimens for suiy, for under-
writing the cost of donating sot- of these to the
U.S. National Museum and othe • nuseums, and
for providing encouragement id numerous
helpful suggestions. Mr. Shin Rong Hwang of
Taipei supplied Mr. Dan with the specimens ob-
tained from the fishing-boat captain, and Mr. T.
C. Lan of Taipei provided information on
associated species. Mr. C. Patrick Nuttall and
Dr. Noel Morris kindly provided access to and
assistance with the fossil collections in the
British Museum (Natural History). Drs. Harald
Rehder and Richard S. Houbrick, Department
of Invertebrate Zoology, Smithsonian Institu-
tion, and Dr. John Pojeta, Jr., U.S. Geological
Survey, Washington, D.('., kindly reviewed the
manuscript and offered suggestions for its im-
provement. My assistant, Mr. Warren C. Blow,
prepared the prints and plates.
LITERATURE CITED
Abbott, R. T. and S. P. Dance. 1982. Cvmperidnim of Sea-
shells. E. P. Button, Inc., New York, ix -i- 411 p.
Boss, K. J. 1982. Mojlusca, p. 945-1166. In S. P. Parker,
Synopsis and Classification of Living Organisms, Vol. 1.
McGraw-Hill Book Co.. New York.
Cox. L. R. 1929. Notes on the Post-Miocene Ostreidae and
Pectinidae of the Red Sea Region, with Remarks on the
46 THE NAUTILUS
Ai»ril 30, 198G
100(2)
Geological Significance of their l)istril>ulio[i. I'mr.
Malacol. Sor. London 18:lfir,-2()9. pis. 11-13.
Eames, F. E., and L. R. Cox. 1950. Some Tertiary Peclina-
cea from East Africa, Persia, and the Mediterranean
Region. Pror. Malacol. Sor. London 32:1-68, 20 pis.
Emerson, W. K. 1965. Strombun (Tricornis) oldi New
Species. Indo-Pncifir MoUuxm l(6):.397-398, pi. 294.
Criiffydd, LI. D. 1981. Observations on the Rate of Produc-
tion of External Ridges on the Shell o{ Pecten marimi/a in
the Laboratory. Jour. Mnrinf Biol. Aax. U.K. 61:401-4 1 1 .
Helm. N. E.. and R. E. Malouf. 1983. Rate of Production of
External Ridges in the Bay Scallop, .4 n/opcc^'H irradtmix.
{.■\bstract) Amer. Zoologist 23(4):1024.
Jones, D. S. 1981. Repeating Layers in the Molluscan Shell
Are Not Always Periodic. Jour. Pateo. 55(5):1076-1082.
Matsukuma, Akihiko. 1978. Fossil Boreholes Made by Shell-
Boring Predators or Commensals. I. Boreholes of Capulid
Gastropods. Jupnnexe Jour. Molncol. lVpnu.-<) 37(l):29-45.
Ohno, Terufumi, 1985. Experimentelle Analysen zur
Rhythmik des Schalenwachstums einiger Bivalven und
ihre Palaobiologische Bedeutung. (Experimental
Analyses Concerning the Rhythm of Shell Growth in some
r^ivalves and its Paleobiological Implications). Pnldconlo-
unipliira. Abt. A, 289:63-123, 7 pis.
Orr, Virginia. 1962. The Drilling Habit or ('apulux daniM
(Crosse) (Mollusea: Gastropoda). The Vrliger 5(2):63-67,
pi. 7.
Waller, T. R. 1969. The Evolution of the Argopi'rtcn gibbux
Stock (Mollusea: Bivalvia). with Emphasis on the Tertiary
and Quaternary Species of Eastern North America.
Polf(„il. Sor. Mfw. 3 (Jour. Palco.. 43(5), suppl.), 125 p.,
7 pis.
1972. The Pectinidae (Mollusea: Bivalvia) of
Eniwetok Atoll, Marshall Islands. The VcIkjct 14(3):
221-264, 8 pis.
1978. Morphology, Morphoclines and a New
Classification of the Pteriomorphia (Mollusea: Bivalvia).
Phil. Trans. Royal Soc. London. B, 284:345-365.
_. 1984. The Ctenolium of Scallop Shells: Func-
tional Morphology and Evolution of a Key Family-level
Character in the Pectinacea (Mollusea: Bivalvia). Malarolo
ijia 25(1):203-219.
A NEW SPECIES OF TRITONIA (NUDIBRANCHIA)
FROM SOUTHERN CALIFORNIA AND BAJA CALIFORNIA
Hans Bertsch'
Biological Sciences, National University, Los Angeles, CA
and
Antonio Mozqueira Osuna
Escuela Superior de Acuacultura, Centro de Estudios Superiores
del Estado de Sonora (CESUES), Navojoa, Sonora, Mexico
ABSTRACT
Tritonia myrakeenae is descrihed as a new species from the Califomian marine
famial province and is ilisfinguished anatomically froni the north Pacific and
north Atlantic species q/" Tritonia.
Although the opisthohranch gastropod fauna
of the northeastern Pacific has been mono-
graphed extensively by numerous authors (e.g.,
recently by Marcus, 19(il a; MacFarland, 19(i(v,
Keen, 1971; McDonald, 1983; et at.), there are
still numerous new distributional records (e.g.,
Bertsch, 1981; Behrens, 1982; Gosliner &
Millen, 1984) and new species descriptions (e.g..
'Mailing address: 6056 Beeman Ave.. No. Hollywood, CA
91606
Gosliner, 1981; Behrens, 1984; and Millen, 1985)
being published. These add significantly to the
known species of opisthobranchs that are
endemic to this coastline or its various marine
faunal provinces, or that are shared with other
marine zoogeographic regions. In this paper we
describe a new species of Tritonia that occurs in
the Californian marine faunal province; the ex-
istence of this species was first reported over 5
years ago (Behrens, 1980).
Vol. 100(2)
April 30, 1986
THE NAUTILUS 47
Order Nudibranchia
Suborder Dendronotacea
Family Tritoniidae Lamarck, 1809
Tritonia myrakeenae Bertsch & Mozqueira,
n. up.
Syno)ii/>ny: Tritonia sp. Behrens, 1980:
102-103 (includes a color photograph of the liv-
ing animal).
Type Locality: Southeast end of Isla Cedros,
Baja California, Mexico, rocky reef west of
lighthouse, in Bahfa Sudeste: 28°2'30"N;
115°12'W.
Type Material: Holotype: Approximately 7
mm long while alive, 4.5 mm preserved; inter-
tidal zone, rocky reef SE end of Isla Cedros; leg.
H. Bertsch and Soa Tsung, 26 December 1985.
Deposited in the collection of the Los Angeles
County Museum of Natural History, Dept. of
Malacology, No. LACM 2135.
Paratype: Approximately 6 mm long while
alive, 4 mm preserved; intertidal zone, rocky
reef SE end of Isla Cedros; leg. H. Bertsch and
Soa Tsung, 26 December 1985. Deposited in the
collection of Los Angeles County Museum of
Natural History. Dept. of Malacology, No.
LACM 2136.
Para types: Three specimens, 3.5, 4, and 4.5
mm preserved lengths; intertidal zone in front
of Hotel Puesta del Sol, El Sauzal, approximate-
ly 8 km north of Ensenada, Baja California,
Mexico (3r52'N; 116°41'W); leg. A. Mozqueira,
September 1984. Deposited in the collections of
California Academy of Sciences, Dept. of Inver-
tebrate Zoology, No. CASIZ 061379.
Additional Records and Range: The authors
and Jesus Pineda have found specimens infre-
quently in the intertidal region at El Sauzal (in
front of Hotel Puesta del Sol), Baja California,
during June, September, October and Novem-
ber 1983, and February and March 1984.
Behrens (1980: 102) reported the occurrence of
Tritonia myrakeenae (as Tritonia sp.) from
"Santa Barbara to San Diego, California." All
known records of this species are only from the
intertidal region. At this time, the known r'ange
of Tritonia myrakeenae is from Santa Barbara,
southern California. U.S.A., to the SE tip of Isla
Cedros, near the southern limit of the state of
Baja California, Mexico.
Description: A thin, elongate, delicate-
appearing tritoniid, 6-18 mm in total length
(alive). Oral veil with 4-7 (rarely branching) ten-
tacular processes. Foot broadly expanded
laterally beyond sides of body; anterior margin
gently rounded, bilabiate; posteriorly extending
out flat past the body, terminating in a pointed
tip. Retractile rhinophores surrounded by basal
sheath; the rhinophore stalk bears 10-22 vertical
processes which encircle the shaft below the tip.
Dorso-lateral edge with a delicate, undulating
free margin from which grow the branchial pro-
cesses (often 9 on each side). Each branchial ap-
pendage branches distally into 3-5 filaments.
Color a very pale dirty orange-brown (see
color photo in Behrens, 1980: 103); oral veil and
sides of foot clear of color, partly opaque. Dis-
tinctive white patches occur on the dorsum
(often as a matched pair on each side of the
midline); Behrens (1980: 103) illustrates an
animal with 4 transverse groups of opaque white
patches (or streaks) arranged down the length
of the back. Specimens from Ensenada and Isla
Cedros (Figiu'e 1) had fewer white splotches
(usually just a pair located about Vs of the body
length distant from the anterior end).
Radula (Figure 2 A) about 1.1 mm long, 0.65
mm across at widest portion. Radular formulae
of 2 specimens collected 26 September 1983 at
El Sauzal were: 22 (10.1.1.1.10) and 25
(8-10.1.1.1.8-10) (widest row damaged but ap-
peared to have 12 outer lateral teeth). Central
rachidian tooth prc.iminent (a|)proximately 63
microns wide), with 3 posteriorly-directed cusps
(Figures 2B and 3B). First lateral tooth well dif-
ferentiated from the others, its structure a
hooklike cusp curling over the side of the rachi-
dian (Figiu'es 2B and 3B). Succeeding laterals
all fairly straight, lilade-like cusps.
Jaws elongate (P^igin-e 3A), each about 1.3 mm
long and 0.37 mm wide; a row of pointed mam-
5 mm
FlCi. 1. Tntiiiiin iiiijrakfi'xiif. xpt'c. tii)i\, dorsal view of liv-
ing animal. Drawing by C. Yanes.
48 THE NAUTILUS
April 30, 1986
Vol. 100(2)
2 A
2 B
FIG. 2. Camera lucida drawings (scale
represents 50(j) of: 2A. Major shape and
features of entire radula, and 2B. Raehi-
dian tooth, innermost lateral, and four
outer lateral teeth of Tri.toiiia niyra-
keenae.
FIG. 3. Tritonia myrakeenae. sketches
of jaws (3A) and selected radular teeth
(3R, rachidian, innermost lateral tooth,
and two outer lateral teeth).
millate denticles begins on the inner margin at
the joined region of the jaws, continuing as a
row along the entire inner edge, increasing
about Va of the length to 3-5 rows; the inner den-
ticled margin terminates distally in a small blunt
process or free flange.
Discusfiion: Tritonia myrakeenae is readily
distinguished from other north Pacific species of
Tritonia. Tritonia hawaiiensis Pease, 1860,
has much more prominent and more highly
branched branchial processes and tints of
orange-pink and dirty light-purple (Bertsch &
Johnson, 1981: 84-85) which are absent in our
new species. Tritonia insulae (Baba, 1955) has
vermilion-tinted gills and a different radular for-
mula: 30 (40-46.1.1.1.40-46). Tritonia diomedea
Bergh, 1894, has a distinct white line bordering
the edge of the foot, and a larger radular for-
mula. Tritonia festiva (Stearns, 1873) has a
series of white lines and loops reticulating on
the dorsum and a radula with more teeth in each
row. Tritonia pickensi Marcus & Marcus, 1967,
has a distinct white swath running down the
center of the dorsum with lateral extensions to
the branchial processes; although it has a similar
radular formula, the shape of the rachidian
tooth (narrower and deeper indentation be-
tween the cusps) and the presence of small den-
ticles on the cusp of the first lateral tooth
(Bertsch & Gosliner, 1984) are differentiating
features.
Species of Tritonia in the North Atlantic are
also easily distinguished from T. myrakeenae.
The tropical T. welhi Marcus, 1961 (b), is pink
and white, and the shapes of the teeth are differ-
ent (cf. Marcus & Marcus, 1967: 100, fig. 130),
and T. bayeri Marcus & Marcus, 1967, has an
opaque white diffuse network over its dorsum.
Tritonia nilsodhneri Marcus, 1983, is rose-pink;
T. m.anicata Deshayes, 1853, has red, black or
olive-green spots on the dorsum; T. plebeia
Johnston, 1828, has white stippling but is darker
colored with brown mottling and has more teeth
per half row (21-33); T. lineata Alder &
Hancock, 1848, has 2 conspicuous longitudinal
white lines running lengthwise down the dor-
sum; although T. homhei-gi Cuvier, 1803, has
white splotches, its body shape is different
(tubercled dorsum, more prominent bilobed oral
veil) and the radula is completely different (den-
ticles on teeth of young specimens and 27-158
teeth in a half row). Thompson & Brown (1984)
give further anatomical characteristics that
distinguish these latter 5 species from T.
myrakeenae. Mrs. Marcus (1983) details the
anatomy of other Tritoniidae, none of which are
comparable with Tritonia myrakeenae.
Etymology: This new species is named in
honor of the distinguished malacologist, Dr. A.
Myra Keen (1905-1986), colleague and friend,
who included nudibranchs in Sea Shells of
Tropical West America, second edition (this was
the first major review of all known nudibranchs
and other opisthobranchs from the Panamic
marine faunal province). Her persistent scholar-
Vol. 100(2
Af)ril 30, 1986
THE NAUTILUS 49
ship and encouragement of research has helped
us to know (and hopefully to protect) the
mollusks of western North America.
Acknowledgments
Field work was partially supported by a grant
(to the senior author) from Have Mule Will
Travel (Alpine, California), and with the co-
operation of the Escuela Superior de Ciencias
Marinas, Universidad Autonoma de Baja
California, Ensenada (Guadalupe Ballesteros,
Director).
We especially thank Jesus Pineda for collect-
ing assistance in Ensenada, and the Cedros
Island Have Mule Will Travel research expedi-
tion team (including Miss Soa Tsung) of
December 1985-January 1986.
The illustration of the living animal of
Tritonia myrakeenae (Figure 1) was drawn by
Senorita Clara Yanes.
LITERATURE CITED
Behrens, D. W. 1980. Pacific coast nudibranchs: a guide to
the opisthobranchs of the northeastern Pacific. Sea Chal-
lengers, Los Osos. 112 pp.
1982. Sakuraeolis en.osimensis (Baba, 1930)
(Nudibranchia: Aeohdacea) in San Francisco Bay. Veliger
24(4):359-363.
. 1984. Notes on the tergipedid nudibranchs of the
northeastern Pacific with a description of a new species.
Veliger 27{l):6b-7l.
Bertsch, H. 1981. Rectification of the generic placement of
Sclewdoris tanyn (Marcus, 1971). comb. tior.. a nudi-
branch from southern California, with a range extension to
the Gulf of California, Mexico. Veliger 23(3):217-220.
Bertsch, H., and T. Gosliner. 1984. Tritoyiin pickeiisi (Nudi-
branchia: Tritoniidae) from Baja California, Mexico. Shells
and Sea Life 16(9):138-139.
Bertsch, H., and S. Johnson. 1981. Hawaiian nudibranchs.
Honolulu, Oriental Publ. Co., 112 pp.
Gosliner, T. M. 1981 . A new species of tergipedid nudibranch
from the coast of California. Jour. Moll. Studies
47:200-20,5.
Gosliner, T. M., and S. V. Millen. 1984. Records oiCuthoria
pustulata (Alder & Hancock, 1854) from the Canadian
Pacific. Veliger 26(3):183-187.
Keen, A. M. 1971. Sea shells of tropical west America, sec-
ond edition. Stanford, California. Stanford University
Press, 1064 pp.
MacFarland. F. M. 1966. Studies of opisthobranchiate mol-
lusks of the Pacific coast of North .-Vmerica. Mem. Calif
Acad. Sci. 6:546 pp.
Marcus. Er. 1961 a. Opisthobranch mollusks from Califor-
nia. Veliger 3 (Suppl.):l-85.
1961 b. Opisthobranchia from North Carolina.
Jour. Elisha Mitchell Scient. Soc. 77:141-151.
Marcus, Ev. du Bois Reymond. 1983. The western Atlantic
Tritoniidae. Bolm. Zool. Univ. S. Paulo 6:177-214.
Marcus, Er. and Marcus, Ev. 1967. American Opisthobranch
Mollusks. Studies Trop. Oceanogr. 6:1-256.
McDonald, G. 1983. A review of the nudibranchs of the Cali-
fornia coast. Malacologia 24(1-21:114-276.
Millen. S. V. 1985. The nudibranch genera Onchidons and
Diaphorodoris (Mollusca, Opisthobranchia) in the north-
eastern Pacific. VV/((/fv28(l):80-93.
Stearns, R. E. C. 1873. Descriptions of a new genus and two
new species of nudibranchiate mollusks from the coast of
California. Proc. Calif Acad. Sci. 5:77-78.
Thompson, T. E., and G. H. Brown. 1984. Biology of
Opisthobranch Molluacs. Volume II. London, The Ray
Society, 229 pp.
UNIONIDAE OF THE UPPER CONNECTICUT RIVER,
A VANISHING RESOURCE'
Arthur H. Clarke
ECOSEARCH, Inc., 325 East Bay view
Portland, TX 78374
Introduction
It was my good fortune to meet William J.
Clench in the winter of 1949-50, shortly after
having become irrevocably committed to shell
collecting. His personality was so enthusiastic
and friendly and the Mollusk Department was so
'In memory of my good friend and teacher, William J.
Clench.
impressive that I soon made frequent trips to
the Museum of Comparative Zoology at Har-
vard, known familiarly as the "MCZ", and later
became a Saturday volunteer. It was not long
after that I resolved to seek a career in
malacology. I shall always be grateful to Bill
Clench and to Ruth Turner for the inspiration to
make that decision and for their numerous acts
of kindness since that time.
50 THE NAUTILUS
April 80, 1986
Vol. 100(2)
I well remember our first collecting trip to the
Connecticut River. The occasion was the 1952
annual field trip of the Boston Malacological
Club; the site was the Connecticut River at
South Hadley, Massachusetts; the leader was
Dr. Clench; the weather was warm and sunny;
and the water was low. Bill, as his friends called
him with affection and respect, led us to a large
sandbar in the middle of the river. Beautiful
mussels were everywhere in 2 or 3 feet of water
and the Lampsilis cariosa were the most
massive that I had ever seen.
During" the following years Arthur and Louise
Clarke collected widely in New England and at
several localities in the Connecticut River
System. There we found Alasmidontu hetero-
don. atrangeAhismidonta uruiulata. and several
other species which, to my neophyte eyes, were
especially marvelous. Although the Connecticut
River fauna had recently been reported upon
(Clench and Russell, 1939, 1940), it still merited
additional investigation. It was not until nearly
30 years had passed, however, that I was able to
do "it.
It is appropriate that the results of that
survey, although principally of regional interest,
should be dedicated to Bill Clench. In a larger
sense, however, all of my research has been in-
fluenced by his teaching and it will always con-
tinue to be so. I would also like to thank The
Nature Conservancy for funding the field work
in 1983 and my wife Judith, and Drs. L. L.
Master and T. French, for valuable field
assistance. Preparation of the manuscript was
supported by ECOSEARCH, Inc.
Methods and Results
The primary objective of the 1983 program
was to determine the present distribution and
abundance of Alasruidovfa hetcrodon (Lea) in
the Connecticut River System of New Hamp-
shire and Vermont. During the course of that
work tabulation of habitat attributes and of the
identity and abundance of all other mollusks en-
countered were also made. The detailed results
concerning/!, keterodori will be reported as part
of a status survey, now underway, of that
species throughout its entire range, but the
general results for 1983 are reported here.
The principle field activities were carried out
over an 18-day period in August and early
September, 1983. Collecting equipment in-
cluded a motor-assisted canoe, wet suits, view-
ing boxes, and a small Kolkwitz dredge. A total
of 36 survey areas were studied. These are
shown in Map 1 and, to conserve space, are ab-
breviated and listed below in narrative form.
Station List: 1, Third Conn. L, E side, N.H.; 2,
Conn R between Third and Second Conn. L; 3,
Second Conn. L, S side; 4, First Conn. L, N side,
N.H.; 5, Conn. R just above Francis L, N.H.; 6,
Conn. R above Canaan, Vt.; 7, Conn. R 1.0 mi N
of Tinkerville, Columbia Twp., N.H.; 8, 9, Conn.
Mass.
FU;. 1. The upper Connecticut River System with 1983
study sites indicated.
Vol. 100 (:;
April 30, 1986
THE NAUTILUS 51
R, by canoe from N Stratford to 2.4 mi above
Stratford, N.H.; 10, Conn. R, 2.4 mi above
Stratford, N.H.; 11, Conn. R, flooded marginal
pool, above bridge at Guildhall, Vt.; 12-14,
Conn. R, by canoe from Comerford Dam to
bridge at Barnet, Vt.; 15, Conn. R, S Newbury,
Vt., V4 mi above Oxbow Bridge; 16, Conn. R, 1.0
mi NW of Piermont, N.H.; 17, Conn. R, Hart-
land, Vt.; 18, Conn. R, Weathersfield Bend, 4 mi
S of Ascutney, Vt.; 19, Conn. R, below bridge
from N Walpole, Vt. to Bellows Falls, N.H.; 20,
Nulhegan R, 0.5 mi W of Bloomfield, Vt.; 21,
Paul Stream, 1.1 mi above mouth, Brunswick
Twp., Vt.; 22, Upper Ammonoosuc R, Groves-
ton, N.H.; 23, Forest L, Dalton Twp., N.H.; 24,
outlet of Hazen's Pond, 2.5 mi E of Whitefield,
N.H.; 25, lake at town park, Thetford Twp., Vt;
26 Mud Pond, Thetford Center, Vt.; 27, Ompom-
panoosuk R, 0.5 mi S of Union Village, Vt.; 28,
Croydon Branch, 1.0 mi S of Croydon, N.H.; 29,
Sugar R, 2 mi SW of Croydon; 30, Williams R,
0.5 mi N of Rockingham, Vt.; 31, Ashuelot Pond
outlet, 3.0 mi NE of Marlow, N.H.; 32, Ashuelot
R, 0.4 mi W of Ashuelot Pond; 33, Asheulot R
just above Marlow, N.H.; 34, Ashuelot R, be-
tween Shaw's Corner and Roundy's Corner,
N.H.; 35, Ashuelot R, 3.0 mi S of Surry Moun-
tain Dam; 36, Ashuelot R, 2.4 mi NW of center
of Keene, N.H.
In most cases living specimens were tabulated
and promptly returned to their habitats. In the
tabulation below, each station number is fol-
lowed by a syml)ol which reflects the number or
abundance of specimens seen there. Numbers of
living (no parenthesis), recently-living (in paren-
thesis), and subfossil (in parenthesis, with S)
specimens are cited separately. Other symbols
are: A = abundant and C = common. No mollusks
were found at stations 4, 5, 6, 12, 13, 14, 20, 22,
24, 27-31, 33, and 34.
Species List
Unionidae. M. inargaritifera: sta. 32, (2S). E.
complnmita: 8,(1S); 15,3; 'l6,(25); 17,ca.500-i-
(77); 18,2-H(1); 19.(5S); 23,12-h(l); 35,A; 36,A.
An. cataracta: l,12-i-(6); 2,6-i-(2); 3,41 -i-(3);
11,(1); 23,2-^(1).^/. heterodon: 17,(5); 35,1-h(2);
36,(1). AL undulata: 1,1 -(-(9); 3,2; 9,(1S); 17,(24);
35,2-^(3); 36,4. St. undulata: 3,1; 17,(4); 35,1;
36,3-f(l). La7rip. r. radiata: 17,ca.300-i-(28);
19,(4S).
Sphaeriidae Sphaerium striafinuni: 17,11.
Viviparidae. Canipclonid decisum: 10,3;
16,27; 17,2; 36,18. Cipanqopaludina chinerhsis:
25, A; 26,A.
Lymnaeidae. Juv. lymnaeid, sp.?: 7, 1.
Physidae. f^hi/.^n heterostropha: 11, A; 16,1.
Planorbidae. Helisovia anceps: 7,1; 8,1; 11,C;
16,4; 17,4.
Ancylidae. Ferrisia rivularis: 9, A; 18, A.
Discussion and Conclusions
According to Johnson (1915), Clench and
Russell (1939, 1940), and Clarke (1981), and
specimen-associated data in the MCZ, USNM,
and ANSP, 10 species of freshwater mussels oc-
curred in the Connecticut River prior to and
during part of the first few decades of this cen-
tury. They are Elliptio complanata, Anodonta
cataracta. An. implicatn. Alasmidonta hetero-
don, Al. undulata. Al. varicosa, Strophitus
undulatus, Lampsilis cariosa, L. ochracea and
L. r. radiata. Three of these (An. implicata, L.
cariosa and L. ochracea) were not known to
ascend the river above Massachusetts. Many
widely-distributed species of Sphaeriidae, proso-
branchs, "and pulmonates were also known to
occur there (Johnson, 1915; Clench & Russell,
1939) and another unionid (Ligumia nasuta) is
also known from the vicinity of Keene, N.H.,
presumably in the Ashuelot River drainage
(Walker and Coolidge, 1908). The principle ob-
jective of this paper is to discuss the unionids of
the main river, but the records listed above from
some tributaries (e.g. the introduced gastropod,
Cipangopaludina chinensis) may also be of
interest.
Early in the course of our work it became ob-
vious that the rnolluscan fauna, and especially
the unionids, of the Connecticut River has been
greatly harmed by human activities. Dams, the
construction of which began in the 1930's, have
altered this once free-flowing river so that it is
now chiefly a series of impoundments within
which water levels are drastically manipulated
by computer controlled dams for the generation
of electricity and for flood control. Pollution
from the pulp and paper industry has further ex-
acerbated the situation. The probable distribu-
tions of the unionids in the upper Connecticut
River, as they existed prior to historical
degredation of the river, are shown in Figau-e 2.
52 THE NAUTILUS
April 80, 1986
Vol. 100(2)
c
<
■D
C
3
■D
C
3
V
(0
4 5"
P
■
•
44'
•
—
4 3'
•
o
• o
•
•
Vt/NH
Mass
FIG. 2. Probable distribution of unionids in upper Connec-
ticut River prior to pollution and impoundment (white bars
and open circles) contrasted with their 1983 distributions
(black bars and black spots). Locations are expressed in
terms of north latitude. Pre-impoundment distributions are
based on subfossil specimens (stations 8 and 19), live
specimens collected by W. .J. Clench from Conn. River near
M(mroe, N.H., and Wells River, Vt., in 1940, other records
at MCZ, I'SNM, and ANSP, and Clench and Russell (1939.
1940).
The di.strihutioii of those species as observed in
1983 are also shown on that figure.
Based on the presence or absence of fresh-
water mussels, it is useful to consider the upper
Connecticut River as now comprised of 3 faunal
regions. Region 1 (stations 1-3) includes the
uppermost part of the system, i.e., the Second
and Third Connecticut Lakes and the interven-
ing portion of the Connecticut River. (The u{)-
permost Fourth Connecticut Lake is small and
inaccessible by road; it was not sampled). Signif-
icantly, the water levels in this part of the
system are not manipulated but are left to fluc-
tuate moderately and naturally. This region con-
tains large poy)ulations oi Anodonta rnturnrta.
(specimens of which have a i)eculiar subarctic
fades), of Alasmidontd undulata morph sower-
hyuna. (an ecophenotyj)e which has been shown
(Clarke, 1981) t<j be attributable to slow growth
in cold, hard-water habitats) and a small popula-
tion of Strophitus undulatus. Elliptio com-
planata does not occur here.
Region 2 (stations 4-14) includes the area from
First Connecticut Lake and Lake Francis down-
stream for more than 100 miles to near the
mouth of the Ammonoosuc River in Grafton Co.,
N.H. Although one apparently fresh pair of
valves of An. cataracta occurred in a flooded
pool adjacent to the Connecticut River (station
11), no freshwater mussels occurred alive in this
whole stretch of the main river. Lakes drained
by at least one tributary (Johns River in Coos
Co., N.H.) do contain both Elliptio complnnata
and An. cataracta, however. Water levels in
First Connecticut Lake and in Lake Francis are
artificially lowered by about 18 feet during the
winter to provide for flood control and water
levels in the Connecticut River throughout
Region 2. They are also drastically manipulated
in response to needs for electric power genera-
tion.
Region 3 (stations 15-19) begins just below
Region 2 and continues, also for more than 100
miles, to near the Massachusetts border. Within
this region water levels are also controlled for
power generation and lake-like impoundments
occur in a nearly unbroken series. With the ex-
ception of one small natural area, in which a
native mussel fauna of at least 5 species still sur-
vives, the fauna throughout the whole region
has apparently been reduced to one species,
Elliptio complanata. The single unspoiled locali-
ty below Sumner's Falls in Hartland, Vt. (sta-
tion 17) is probably the site of the several
historical records from Hartland (see Johnson,
1915). Here the river tumbles over a broad
escarpment and, some distance below the falls
where reoxygenated water loses its turbulence,
a small population oi Alasmidonta heterodon ex-
ists and large populations of other species still
flourish. Convenient access here is only possible
by boat and then only during the infrequent and
unpredictable periods of computer permitted
low-flow. It is hoped that this inaccessability will
contribute to the survival of A. heterodon here
and to the conservation of the unusually healthy
mussel community in which it occurs.
It is interesting that the ubiiiuitous and abun-
dant species Elliptio comphmato is entirely
absent from Region 1, a situation which we first
Vol. 100(2)
April 80, 1986
THE NAUTILUS 53
ol)served in 1955. To my knowledge there are
few other substantial areas within the g-eo-
graphical range of that species (northern
Ontario and Nova Scotia to Georgia), where
ecological diversity occurs and mussels are
found, which do not contain E. coniplanata. It
appears probable that the absence of E. coni-
planata is attributable to the inability of its only
known host fish, the ye'low perch, to ascend the
turbulent and shallow portion of the Connecti-
cut River below the Second Connecticut Lake.
In summary, our work has indicated that the
upper Connecticut River now supports mussel
populations of good species diversity in only two
small areas, viz. the uppermost Connecticut
Lakes and their vicinity, and an unusual locality
at Hartland, Vt. Other work in 1983, which is
still incomplete, demonstrates a similarly bleak
but uneven situation for the lower Connecticut
River. The diverse mussel community at South
Hadley, Massachusetts, which we observed in
1952 is now gone and only a few specimens of
Ellipflo complanata now occur there. A healthy
molluscan community containing E. covtphntn-
ta. An. rataracta, A)h iniplicafn. and AI. U7i-
ihiUitii and the pleurocerid GiDiinbusis virginicd
still occurs in a short reach of the Connecticut
River from the southern l^order of Massachu-
setts to Warehouse Point, Connecticut,
however.
Clearly the mussel fauna of the whole Connec-
ticut River now survives in only a very few
remnant communities. Conservationists and
government agencies are urged to help in
reversing this unfortunate trend toward
extinction.
LITERATURE CITED
Clarke, Arthur H.. 1981. The Trilie .Alasmidontini
(Unionidae: Anodontinae), Part 1; Piyuis, Atasmidonta.
and Arridpris. Smithsovinn ('imtrihutions to Zoology,
No. 326.
Clench, W. J. and H. 1). Russell. 1939. Freshwater Shells of
New Hampshire. Bioloyical Surivy of the Merrimuck
Watfrsihed. New Hampshire Fish and Game Department,
Surve.v Report No. 3, pp. 201-206.
1940. Freshwater Shells of New Hampshire. The
NautUw! 54:52-53.
Johnson, Charles W., 1915. P\-iuna of New England. List of
the Mollusca. Uccii!<i(iiiol I'npfrx of the Bustoti Society of
Natural History, vol. 7, part 13.
Walker. R. D. and W. H. Cooli<lge. Jr.. 1908. Mollusca of
Keene. New Hampshire. The NmitihiK 22:32.
MORPHOLOGICAL ANOMALIES IN THE SHELL OF
FIELD-COLLECTED BIOMPHALARIA GLABRATA (SAY, 1818)
Jose Gomez, Mercedes Vargas
Departamento de Microbiologia y Parasitologia
Universidad Autonoma de Santo Domingo
Dominican Republic
and Emile A. Malek
Department of Tropical Medicine
Tulane University Medical Center
New Orleans 70112-2699
ABSTRACT
We report the occurrence of phenotypic abnormal shelU of the freshwater .swj.i/
Biomphalaria glabrata (Stt^, 1818) in different habitats, actual and potential foci
of transmission of schistosomiasis mansoni. in the Dotninican Republic. There is
the possibility that genetic factors cafuae the abnormalities in the shell, and that
they are inherited through cross-fertilization.
Introduction
During the normal growth of a shell of a com-
mon planorbid snail it increases in diameter in
the same plane, by the addition of new whorls
one at the side of the other resulting in a dis-
coidal form (planispiral). Sometimes, however,
this growth process shows anomalies which pre-
sent the malacologist with problems in the iden-
54 THE NAUTILUS
April 80, 1986
Vnl. 100(2)
TAl-iLK I. I 'ri'valencc i)f abiKirmai shi'lls aiiKing natural
populations of Biomfihiilnriti gliiltralii in the Dominican
Republic.
No.
No,
(%)
No. shells
normal
abnormal
Locality
examined
shells
shells
Higuey
124
111
13
110 4)
Sabana de la
Mar
209
182
27
(13)
Nisibon
46
46
0
Haina
156
153
3
(2)
Jarabacoa
48
44
4
(8.3)
Hato Mayor
226
212
14
16)
San Francisco
de
Macoris
25
24
1
(41
tification of a particular species. Richards (1970,
1971) observed adult BiomphaUirin gluhmtn
with projecting spires in genetic stocks showing
frequent embryos with the first whorl open, and
with high eml)ryonic mortality. Phenotypic
anomalies in the shell have also been reported by
Andrade and Carvalho (1973) in B. straminea
(Dunker, 1848) raised in the laboratory in Brazil
and by Gomez (1973) in B. glabnUa collected in
the Dominican Republic. Andrade and Carvalho
stated that deformation of the last whorl was
the most frequent anomaly, while Gomez
observed abnormalities of various types.
In this paper we report on phenotypic defor-
mations in the shell of 5. glabraUx in populations
occurring in various actual and potential foci of
transmission of schistosomiasis mansoni in the
Dominican Republic. A total of 834 shells were
examined and they were obtained from the fol-
lowing localities: 124 from Higuey, 209 from
Sabana de la Mar, 46 from Nisibon, 156 from
Haina, 48 from Jarabacoa, 226 from Hato
Mayor, and 25 from San Francisco de Macoris.
Results
As shown in Table 1, of 124 snails collected in
Higuey 13 demonstrated conchological anoma-
lies for a prevalence of 10%. Among 209 snails
which came from Sabana de la Mar, 27 (13%)
were abnormal, whereas those from Nisibon did
not show any deviations. Three of the 156 snails
collected in Haina exhibited shell abnormalities,
as well as 4/48 from Jarabacoa, 14/226 from
Hato Mayor, and 1/25 from San Francisco de
Macoris.
The most frequent anomaly was the deflection
of the last whorl to the left and the inclination of
the preceding whorl to the right (Fig. 1). In
some shells the deflection of the last whorl was
pronounced to about 180°, in such a way that
4# A
mm
FIG. 1. liiniiiphdldnii (iliihriitii froni the Doniinican Republic. Top row; normal shells, left
(under or umbilical) side. Middle row; abnormal shells, left (under or umbilical) side. Bottom
row; abnormal shells, rinht (upper) side.
Vol. 100(2)
April 30, 1986
THE NAUTILUS 55
the aperture was detached from the preceding
whorl, giving the shell a helicoidal api)earance.
As a result the early whorls overlapped, and the
umbilicus became much narrower than in nor-
mal shells. In addition to the abnormalities in
the form of the shell it was common to observe
the deposition and incrustation of calcareous
material in the abnormal shells. Scarifications of
the umbilicus were never observed.
Discussion
Sturrock and Sturrock (1971) showed that in
St. Lucian B. glabrata infected with Schisto-
soma mansoni there is a pronounced distortion
of the aperture to the right (upper) side, that is,
distortion in the opposite direction from that of
the shells we are reporting upon from the
Dominican Republic. The distortion in the in-
fected snails reported by the above authors,
evidently resulting from anatomical changes
due to the infection rather than being genetical,
first appeared at the end of the prepatent period
of the infection and were associated with the
liberation of cercariae from the snail.
In his studies on the genetics of B. glahrata.
Richards (1970, 1973) indicated that five single
gene characters have been demonstrated, name-
ly, basic pigmentation, pearl formation, antler
tentacles, everted preputium and swollen tenta-
cles, and adult insusceptibility to infection with
S. mansoni. In addition to the above, several
multifactorial inherited growths have been
observed including pulmonary cavity growths,
tentacle and eye variations and median head
bulbs. Other multifactorial genetic characters
include ajiertural lamellae, spire formation
(Richards, 1971), mantle pigment and suscepti-
bility of juvenile B. glabrata to infection with S.
mamoni (Richards and Merritt, 1972). The
presence of abnormal shell growth in different
natural populations of B. glabrata in the
Dominican Republic suggests that genetic fac-
tors cause the formation of these anomalies. The
alisence of such factors in certain populations
(Nisibon) and their low frequency in others may
indicate their association with a sublethal gene
whose penetration may inhibit high frequencies.
However, cross-breeding experiments are
needed to determine the validity of this specu-
lation and the type of genetical inheritance in-
volved in the formation of abnormal shells.
LITERATURE CITED
Andrade, R. M. and Carvalhu, C. S. 1973. Aiiomalias en
conchas de Biamphaldrin straminen (Dunker. 1848),
criadas en laboratorin (Pulmonata. Planorbidae). Rev.
SaudePuhlica (S. Pniilo) 7:28.3-284.
Gomez. .1. 197.3. Distrihucion geografica del Birmiphiilaria
gliibrata (huesped intermediario del Sc/N.sfo.sowK miDhsorii)
en Republica Dominicana. Tke^ix for Licenciado en
Biologia, Universidad Autononia de Santo Domingo.
Richards. C. S. 1970. Genetics of a molluscan vector of schis-
tosomiasis. Nature 227:806-810.
1971. Biiimphalnriri (jUihnitu genetics: .Spire for-
mation as a sublethal character. Ji>iir. Inrert. Pnth.
17:.53-i58.
1973. Genetics of Bior/ijihulnrin glahmta (Gas-
tropoda: Planorbidae). Mtilaeol. Reriew 6:199-202.
and Merritt. J. W. 1972. Genetic factors in the
susceptibility of juvenile Bumiphalnrin qlabrnta to
Schistosomii in<ntxi)ni infection. Aiiiei'. ■Imir. Trap. Mnl.
Hyg. 21:425-434.
Sturrock, R. F. and Sturrock, B. M. 1971. Shell abnormali-
ties in Biomphalnriii gliibnila infected with .Sf/(i.s(o.somfi
//(((H.s-on/ and their significance in field transmission
studies, .in// r. Hehiiiiith<il. 45:201-210.
NEW MOLLUSK JOURNALS
Heldia, Miinchner Malakologische Mitter-
lungen, a West German mollusk journal, under
the editorship of Gerhard Falkner (ISSN
0176-2621) was launched in 1984. Annual sub-
scription is DM 25 (about U.S. $12.00). Write:
Postfach 26 01 23, 8000 Munich, West Germany.
Most articles in Band 1 have been on land and
freshwater moUusks, but some new marine
species are described {Conus montillai Rockel,
1985).
A-pex. Informations Scientifiques de la Societe
Beige de Malacologie (a quarterly), vol. 1. n<i. 1,
36 pp., 3 pis. Editor: R. Duchamps. Annual
suliscription of 900 B.F. for Apex and Arion
(their news and popular publication) should be
sent by international money order or bank check
in Belgium Francs to: M. J. Buyle, Av. M.
Maeterlinck, 56, bte 8, Bruxelles, Belgium
B-1030. The first numlier contains new marine
Rumanian gastropods by Grossu and new
Australian X'olutidae by Foppe.
56 THE NAUTILUS
April 80, 1986
Vol. 100(2)
THE ECOLOGY OF FRESHWATER GASTROPODS
IN THE CENTRAL CANADIAN REGION
Eva Pip
Department of Biology
University of Winnipeg
Winnipeg, Manitoba
Canada R3B 2E9
ABSTRACT
The ecology of frefihwater gastropods was surveyed at more than 1,00 permnnent
aquatic habitats located within the area bounded by 47° and 54° N and H° and
106° W during 1972 to 1984. Parameters examined were: water body type, sedi-
ment type, gastropod community diversity, submerged macrophyte diversity, sur-
face water pH, total dissolved solids, total alkalinity, chloride, sulphate, nitrate/
nitrite and soluble reactive phosphorus. Many species showed distributioTis with
respect to these parameters that differed from the total site sampling distribu-
tions. Gastropods in the study area appeared to form a continuum according to
habitat type, with Stagnicola palustris, Physa jennessi and Fossaria modicella at
the higher extremes of water chemistry, and S. reflexa, Bulimnea megasoma,
Marstonia decepta and Helisoma campanulatuni at the lower end of the scale.
Species able to tolerate high dissolved inorganic values also showed broad
tolerance ranges for these parameters. Regional variation in tolerance ranges
may be a com ple.r function of adaptation combined with the inter-relationsihips
between various aspects if the habitats themselves.
The physical environment is believed to ac-
count for much of the observed distribution pat-
terns of freshwater gastropods (e.g. Aho, 1966).
The environmental factors governing molluscan
occurrence have been the sulyect of many
studies in various parts of the world. Of par-
ticular importance have been the contributions
of Macan (1950, 1957) and Dussart (1976) in
England, Okland (1979) in Norway and Aho et
al. (1981) in Finland. In North America much
ecol(jgical intVirmation has been presented by
Ilarman and Berg (1971), Clarke (1973, 1981),
Pip (1978, 1985) and others.
Various aspects of the aquatic environment
may influence snail distributidii, for example
water chemistry, degree of water flow or tur-
bulence, water body size, substrate type and
biotic factors such as type and abundance of
aquatic vegetation and composition of the
gastropod community (as competition may be a
factor, e.g. Aho et al. (1981)). 'i'lie problem is
complicated further in that local differences
may exist in the tolerance ranges of a given
species with respect to a particular parameter.
and thus the relative importance of different
parameters may show regional variation (Pip,
1985). However, such variation is difficult to
detect and evaluate since few data are available
in the literature in consolidated form regarding
the ecological characteristics of individual
species in different geographical areas.
The present paper presents the results of
ecological surveys carried out from 1972 to 1984
at more than 400 permanent aciuatic habitats
located within the area bounded by 47° and
54°N and 94° and 106°W (eastern Saskat-
chewan, Manitoba, northwestern Ontario,
northern North Dakota and Minnesota), with
sampling locations being more concentrated in
the eastern portion of this area. The parameters
examined included water chemistry (pH, total
dissolved solids, total alkalinity, chloride,
sulphate, nitrate and nitrite, and soluble reac-
tive phosphorus), water body size and type,
substrate type, and diversity and species com-
position of the gastropod and submerged
acjuatic macrophyte communities. Analyses of
the latter parameter, i.e. community composi-
Vol. 100 (L
April 80, 1986
THE NAUTILUS 57
tion, have lieen reported elsewhere (Pip, 1978,
1985).
Materials and Methods
Surveys were conducted during May to
Sejitember of each year. All sites sampled con-
tained water year-round and aquatic communi-
ties appeared established. Most of the sites were
sampled only once. However 11 sites throughout
the region were monitored for water chemistry
parameters at 2-week intervals during an entire
sampling season in order to estimate the range
of seasonal variation at a given type of site. Ap-
proximately 50 additional sites were scored for
all parameters at least twice in different years.
At each site all species of snails encountered
while wading or canoeing within a search time
of 1 hour were recorded. Sul)merged plants
were collected by hand and by dredging with a
rake; these were taken to the laboratory,
washed and examined for additional snails.
Plant community diversity was scored Ijy in-
cluding only plants that were at least partially
sul)merged. Large water bodies were sampled
at a number of stations and each was treated as
a separate site because of the heterogeneity of
such waters.
A surface water sample was collected at each
site, immediately placed on ice in a lightproof
container and frozen within a maximum of 48
hours after collection. The water chemistry
parameters were determined on the thawed
samples using methods recommended by the
American Public Health Association (1972). The
pH was measured directly in the field using a
portable pH meter.
When compiling the water chemistry data, if a
number of water chemistry values were avail-
able for the same site, the two extreme values of
each parameter at that site were included in the
tolerance range of the species which occurred at
such a site.
Results
A total of 38 species was identified as occur-
ring at two or more water bodies within the
study area. In addition to these identifiable
species, a number of Physa lots were collected
whose identity could not be established. These
were of several morphological types, each of
which was present at a number of sites.
Water body tyjie was classified according to
area, if lentic, or depth, if lotic (Table 1). The
most heterogeneous group was that of ponds;
this group included water bodies of various
origins and basin types, such as natural ponds,
oxbows, artificial excavations (ditches, farm
ponds, (juarry pits, road fill excavations, etc.),
I)eaver ponds, spring fed pools and bog pools.
Many gastropods appeared to show distribu-
tions which were markedly different from the
overall site sampling distribution. In all subse-
quent discussion, only species for which N>5
will be considered. Although almost all species
could occur in lakes, this water body type was
the major type of habitat for all of the amni-
colids, and ValiHita spp., Stagnicola catasco-
pium, Fossaria decampi and Helisoma carnpa-
nulatum. Ponds were the major water body type
for Stagnicola caper ata, Fossaria exigua,
Planorbula campestris, Armiger crista, and to a
lesser extent, Stagnicola palustris. Aplexa
hypnormn and Physa jennessi (ssp. skinneri
Taylor, 1953). Bulim.nea megasowM appeared to
favor rivers above other habitat types when
compared to the overall sampling distribution.
In general, running waters were preferred over
lentic habitats by Stagyiicola rejlexa. Bulimnea
megasoma. Ferrissia rivularis and Planorbula
armigera. Gyraulus deflectus occurred often in
both running waters and lakes but appeared to
avoid ponds.
Distribution of gastropods with respect to
substrate type (Table 2) showed that Ferrissia
rivularis and Stagnicola reflexa were commonly
found in granitic Precambrian Shield basins,
although they also occurred on clay and coarse
sediments respectively. Planorbula campestris
occurred mostly on coarse and silt sediments.
Sand appeared to lie preferred by Valvata
since7'a. V. tricarinata., Cincinnatia cincinna-
tiensis. Marstonia decepta. Probythinella
lacustris, Stagnicola catascopium, Fossaria
decampi, Helisoma campanulatum and Pro-
nienetiis umbilicatellus. Fossaria exigua and
Stagnicola caperata favored both sand and clay,
while clay was the major sediment type for
Stagnicola. palu.stris, Fossaria modicella and
Helisoma pilsbryi. Physa jennessi preferred
both silt and clay. Physa gyrina, Lymnaea
stagnalis. Helisoma anceps, H. trivolvis, Planor-
bula armigera and Gyraulus parvus appeared to
58 THE NAUTILUS
April 80, 1986
Vol. 100(2)
TABLE I . Percc'ntai;<' ciislriliiiti<in accunliiif; t" haliitat tyin' in the stiuly area. N = no. ot'i)l)sena-
tions.
Species
Lakes Ponds Rivers Creeks N
>10 ha <10 ha -Zm deep '2ni deep
Campeloma decisum Say, 1816
Valvata sincere Say, 1824
V. tricarinata Say, 1817
Cincinnatia cincinnatiensi s
Anthony, 1840
Marstonia decepta F.C. Baker,
1928
Probythinella lacustris F.C.
Baker, 1928
Amnicola 1 imosa Say, 1817
A^ walkeri Pilsbry, 1898
Lymnaea staqnal is Linne, 1758
Acella haldemani "Deshayes"
Binney, 1867
Bui imnea megasoma Say, 1824
50
50
57
29
84
14
2
73
4
23
100
86
71
80
40
100
30
Stagnicola palustri s Muller, 1774 29
S_. catascopium Say, 1817
S^ caperata Say, 1829
S^ reflexa Say, 1821
Fossaria da11i F.C. Baker, 1907
1896
92
14
29
50
75
7
35
20
47
36
22
F. decampi Streng,
F. exigua Lea , 1841
F. modicel 1 a Say, 1825
F^ parva Lea, 1841
Physa qyrina Say, 1821
P^ jennessi Dall, 1919
Aplexa hypnorum Linne, 1758
Ferrissia paral lela Haldeman,
1841
F_^ rivularis Say, 1817 45
Hel isoma trivolvis Say, 1816 42
H. pi 1 sbryi inf racarinatum
F.C. Baker, 1932 42
FL corpulentum Say, 1824 50
ti. campanulatum Say, 1821 81
H^ anceps Menke, 1830 47
Planorbula arniigera Say, 1821 41
P^ campestris Dawson, 1875 29
Promenetus exacuous Say, 1821 51
P. umbili eaten us Cockerell, 1887 43
Armiger crista Linne, 1758 33
Gyraulus parvus Say, 1817 43
G^ circumstriatus Tryon, 1866 41
G. deflectus Say, 1824 59
14
4
7
44
26
14
7
7
19
3
69
20
5
47
6
7
246
3
35
26
9
23
57
6
8
170
8
12
86
7
29
29
13
7
25
25
4
12.5
12.5
8
86
7
14
52
9
4
46
80
5
36
10
7
253
58
6
33
62
5
11
37
100
3
19
23
13
31
43
7
8
189
37
21
19
50
4
4
15
75
44
3
6
106
29
16
14
68
71
7
31
11
7
55
43
14
7
67
9
45
5
7
161
48
4
7
27
16
14
11
44
TOTAL SITES
40.5
43.0
9.0
7.5 412
be substrate-indifferent.
The mean gastropod community diversities
where each species was found were higher than
the mean overall site diversity (Table 3) because
all species except Sfngnicola rcjlexa occurred to
some extent in a proportion of highly diverse
comnuinitii's. For species with N>5, Fossaria
ilcrnmiii and Frohnthinclla hirustris. both
primarily lacustrine species, showed the highest
diversity values. Low mean (liversities were
seen for communities in which Stagnicola
rejlexa, Ferrissia rivularis. Physa gyrina. Stag-
Vol. 100(2) April 30, 1986
TABLE 2. Perceiitaije ilislriliutimi acconiing to sul)strate type in thf study area.
THE NAUTILUS 59
Species
Gravel/
Bedrock coarse
Granitic Litnestone Shale sand
Sand Silt Clay Organic
Campeloma decisum
75
25
4
Valvata sincera
14
57
29
7
V. tricarinata
4
2
11
46
2
20
15
46
Cincinnatia cincinnatiensi s
15
4
62
19
26
flarstonia decepta
88
12
8
Probythinel la lacustris
29
57
14
7
Amnicola limosa
19
12
39
1
16
13
69
A. walkeri
33.3
33.3
33.3
6
Lymnaea stagnalis
6.5
2
1
17
24
6.5
23
20
246
Acella haldemani
100
3
Bulimnea megasoma
19
19
24
14
24
21
Staqnicola palustris
2
2
2
21
23
9
29
12
172
S. catascopium
8
8
8
50
18
8
12
S. caperata
57
43
7
S. reflexa
43
43
14
7
Fossaria dalli
50
25
25
4
F. decampi
12.5
75
12.5
8
F. exiqua
7
7
43
7
36
14
F. modicella
2
2
2
13
22
11
34
14
45
F. parva
20
20
20
40
5
Physa gyrina
12
2
1
15
28
5
22
15
251
P. jennessi
9
21
21
34
15
33
Aplexa hypnorum
3
3
34
18
5
26
11
38
Ferrissia parallela
33
67
3
F. rivularis
37
7
13
33
10
30
Helisoma trivolvis
4
2
1
18
24
9
25
17
189
H. pilsbryi inf racarinatum
16
4
32
32
16
19
H. corpulentum
25
25
50
4
H. catnpanulatum
16
1
10
49
4
6
14
73
H. anceps
8
19
28
2
19
24
107
Planorbula armijera
9
3
3
15
21
3
24
22
67
P. campestris
43
14
29
14
7
Promenetus exacuous
15
4
13
16
7
29
16
55
P. umbilicatellus
14
14
58
14
7
Armiger crista
11
23
33
33
9
Gyraulus parvus
5
1
1
16
26
9
21
21
161
G. ci rcumstriatus
8
4
23
34
4
8
19
26
G. deflectus
12
2
9
35
5
12
26
43
TOTAL SITES
10.8
2.0
0.9
15.9
27.0
5.9
19.6
17.9
408
nicoln pdlusfris, Lymnaea stagnalis, Helisoma
anceps. Bulimnea m.egasnma. Physa jennessi.
Fossaria exigua and Helisoma trivolvis were
present. The maximum ret-onled gastro|)od
community diversity was 17.
Mean macrophyte community diversity was
high for Valvata sincera. Gyrauluji deflectus.
Hciisonut campanulatum, Bulimnea megasonta
and all amnicolids except Prohythine.lla
lacuMris. Low mean macrophyte diversities {<6)
were seen for Physa jennessi, Fossaria modi-
cella, Probythinella laciistris. Fossaria exigua.
Stagnicola palustris and S. capcrala. Of tlie
above species, mean diversity values were low
for both gastropod and macrophyte communi-
ties for Physa, jennessi. Fossaria exigua and
Stagnicola i)alu.'<fris. As has previously been
noted by Pip (1985), there was little correlation
between the two kinds of diversity at the dif-
ferent site types, aside from the tendency of
ponds to contain few species of both snails and
plants.
The widest range for surface water pH was
observed for Helisoma trivolvis (5.5 pH units,
equal to the total sampling range) (Table 4),
followed by H. fnireps. Ferrissin rivularis,
60 THE NAUTILUS
Ai)ril 80, 1986
Vol. 100(2)
TABLE 3. Moan trastnip"<l ami suliiiiei'f;tMi macniphyte divorsily of ccimiminities in which each
species was found in the study area.
Species
Gastropod
diversity
N
Macrophyte
diversity
N
Campeloma decisum
13.3
3
17.3
3
Valvata sincera
9.6
7
10.4
7
V. tiicarinata
8.3
46
8.1
46
Cincinnatia cincinnatiensis
7.7
27
12.2
25
Marstonia decepta
7.3
8
14.6
8
Probythinella lacustris
10.0
7
5.0
7
Amnicola limosa
7.7
68
10.6
68
A. walkeri
6.0
5
11.6
5
Lymnaea stagnalis
5.5
246
6.9
246
Acella haldemani
11.0
3
16.7
3
Bulimnea meqasoma
5.6
21
10.1
19
Stagnicola palustris
5.5
173
5.4
166
S. catascopium
9.2
13
6.4
11
S. caperata
6.1
7
5.8
6
S. reflexa
4.0
7
9.9
6
Fossaria dalli
7.8
4
8.0
4
F. decampi
11.0
8
8.1
8
F. exiqua
5.8
14
5.4
13
F. modicella
7.1
47
5.0
44
F. parva
6.6
5
5.0
5
Physa gyrina
5.4
250
7.3
246
P. jennessi
5.7
33
4.8
31
Aplexa hypnorum
6.7
36
6.2
33
Ferrissia parallela
10.5
2
17.0
2
F. rivularis
5.3
31
7.6
30
Helisoma trivolvis
5.8
189
7.0
189
H. pilsbryi inf racarinatum
7.2
19
9.0
18
H. corjjulentum
5.0
4
9.5
4
H. campanulatum
6.4
74
11.6
73
H. anceps
5.6
108
7.2
102
Planorbula armigera
6.7
68
8.5
63
P. campestris
7.7
6
3.7
6
Promenetus exacuous
7.7
55
7.6
65
P. umbilicatellus
4.9
7
8.9
7
Armiger crista
9.7
9
3.8
9
Gyraulus parvus
6.0
165
7.2
158
G. circumstriatus
6.6
27
7.5
27
G. deflectus
7.3
44
11.7
41
TOTAL SITES
4.6
403
6.8
397
Gyraulus dejlertus, Stagnix'olu palusinx,
Fossaria rnodicella and Gyraulus parvus (all at
> 4 pH units). The narrowest ranj^es (< 2 units)
were seen for Planorbula campestris, Mar-
stonia decepta and Fossaria decampi; these
three species liowever were sampled at relative-
ly few sites. The highest sampled pH of \()Ji was
tolerated by Stagnicola palustris, Fassaria
modicella, Helisoyna trivohns, Promenetus
exacuous, Aryniger rj-ista and Gyraulus parvus,
while the lowest uH of 5.0 was observed for
Bulimnea megasonia. Ferrissia rivularis,
Helisoma trivolvis, H. anceps and Gyraulus
dejlertus.
The widest ranges for total dissolved solids,
encompassing nearly the total range sampled,
were seen for Fo.nsaria modicella. Stagnicola
fiatustris and Physa jennessi (Table 4), followed
by somewhat smaller ranges (approx. 4500 mg/1)
for Lymnaea. stagyialis and Helisoma trivolvis.
Narrow ranges (300 mg/1 or less), all towards
the bottom end of the scale, were seen for
Vol. 100(2)
April :;o, i;)S6
THE NAUTILUS HI
TABLK 1. Minimuni. iikixiiiiuiii ami luraii \aliK'S fcir pH ami tutal disscilvt'd solids for ffaslnipods in
the stud\ area.
Species
pH Total
dissolved solids, mg/1
Min. Max. x H Min. Max. x H
Campeloma dec i sum
7.1
8.1
7.8
3
58
123
87
3
Valvata sincera
6.2
9.2
7.4
6
134
384
264
6
v. tricarinata
6.7
9.8
8.3
48
33
1794
432
47
Cincnnnatia ci nci nnat lens i s
7.3
9.8
8.3
25
33
875
170
24
Marstoma decepta
7.7
9.2
8.4
9
60
208
134
7
Probythinel la lacustris
7.9
9.5
8.5
5
104
1300
494
5
Amnicola limosa
6.1
9.8
8.1
80
16
1794
235
79
A. wall<eri
7.0
9.0
7.9
6
55
219
99
5
Lymnaea staqnalis
6.2
10.0
8.1
260
16
4549
337
255
Acella haldemani
7.4
8.5
8.0
3
68
143
111
3
Bulimnea meqasoma
5.0
9.0
7.2
29
16
271
93
29
Stagnicola palustris
6.2
10.5
8.2
174
38
5533
535
170
S. catascopium
7.3
9.5
8.6
12
37
1300
509
11
S. caperata
6.6
8.4
7.8
3
196
919
504
3
S. reflexa
6.6
8.8
7.7
7
16
80
58
7
Fossaria dalli
7.5
8.3
7.8
3
89
280
212
3
F. decampi
7.9
9.5
8.6
6
104
1300
354
6
F. exiqua
6.6
9.8
7.8
14
129
1763
371
13
F. modi eel 1 a
6.2
10.5
8.3
49
33
5533
751
47
F. parva
6.7
9.5
8.1
4
152
1596
565
4
Physa gyrnna
6.1
10.1
8.0
267
16
2399
272
261
P. jennessi
7.1
10.5
8.4
28
60
5533
799
28
Aplexa hypnorum
6.6
9.5
7.8
35
37
1402
424
35
Ferrissia parallela
7.1
7.3
7.2
2
78
219
149
2
F. rivularis
5.0
9.5
7.6
38
15
1300
169
37
Helisoma tnvolvis
5.0
10.5
8.0
197
16
4549
345
196
H. pilsbryi i nf racari natum
6.6
9.5
7.7
15
16
743
169
15
H. corpulentum
8.0
8.4
8.2
5
42
80
57
5
H. campanulatum
6.9
9.5
8.1
91
30
334
104
89
H. anceps
5.0
9.8
8.0
113
18
1333
237
111
Planorbula armigera
6.2
9.7
7.8
68
16
1794
339
67
P. campestris
7.5
8.8
7.9
6
138
459
273
6
Promenetus exacuous
6.9
10.5
8.2
60
40
1794
413
60
P. umbi 1 icatel lus
6.7
9.4
8.1
6
80
734
267
6
Armiger crista
7.3
10.5
8.4
10
219
1794
836
10
Gyraulus parvus
6.2
10.5
8.1
176
24
2399
317
172
G. CT rcumstriatus
6.6
9.8
8.3
26
18
2108
418
26
G. deflectus
5.0
9.4
7.8
48
32
1571
176
47
TOTAL SITES
5.0
10.5
8.0
446
10
5533
302
440
Stagnicola reflexa, Marstonia decepta. Valonta
fiincera, Bulimnea m.egaso»ia and Helisoma
campanulatum.
Total alkalinity ranges (Table 5) were widest
(> 700mg/l CaCOj) for Stagnicola palustris.
Gyraulus deflectus, G. circumstriatus and
Physa jennessi. Narrow ranges (<100 nig/l
CaCOs), all again towards the bottom end of the
scale, were seen for Stagyiicola reflexa and
Valvata sincera. both of which were repre-
sented by small numbers of samples. Thirteen
species occurred at alkalinity values as low as
0-4 mg/1 CaCOa, while only three were observed
at the maximum sampled value of 800 mg/1
CaCOs.
All species tolerated chloride values of 0 mg/1
(Table 5), but only Stagnicola palustris,
Fossaria modicella and Physa jennessi could be
found throughout the complete range sampled.
Valvata sincera and Stagnicola reflexa ap-
parently avoided chloride altogether, although
again these were represented by small sample
numljers. Fossaria decampi and Marstonia
decepta showed chloride ranges of < 10 mg/1.
62 THE NAl'TILUS
April 30, 1986
Vol. 100(2)
TABLE 5. Mininiuiii. niaxinium and mi'aii valufs tor total alkalinity and chloridi- for tjastrupods in
the study area.
Species
Total
alkal
i ni ty .
, mg/1
)
Chloric
le, mg/1
CaCO.,
Min.
Max.
" X
N
Min
. Max.
x
N
Campeloma decisum
64
128
97
3
0
0
0
3
Valvata sincera
70
166
119
6
0
0
0
6
V. tricarinata
0
448
144
47
0
480
70
47
Cinci'nnatia cincinnatiensis
14
239
91
24
0
18
3
23
Marstonia decepta
70
220
122
8
0
8
1
8
Probythinel la lacustris
70
159
132
5
0
238
48
5
Amnicola limosa
4
448
96
78
0
480
34
77
A. walkeri
11
172
63
5
0
8
2
5
Lymnaea stagnalis
0
560
135
255
0
592
25
254
Acella haldemani
72
100
81
3
0
0
0
3
Bulimnea megasoma
9
172
54
29
0
56
3
28
Stagnicola palustris
4
800
180
172
0
1234
51
172
S. catascopium
84
184
134
11
0
430
130
11
S. caperata
106
224
173
3
0
7
2
3
S. reflexa
0
72
31
7
0
0
0
7
Fossaria dalli
72
202
129
3
0
4
1
3
F. decamgi
70
284
138
6
0
2
0.
3 6
F. exigua
36
560
183
13
0
77
10
13
F. modicella
48
448
194
48
0
1234
115
48
F. parva
108
230
167
4
0
21
5
4
Physa gyrina
0
560
122
263
0
592
24
262
P. jennessi
62
768
196
28
0
1234
79
28
Aplexa hypnorum
4
448
179
33
0
438
17
33
Ferrissi'a parallela
128
172
150
2
0
0
0
2
F. rivularis
4
220
68
38
0
238
9
37
Hell soma trivolvis
0
654
144
195
0
480
22
195
H. pilsbryi inf racarinatum
10
316
106
15
0
261
18
15
H. corpulentum
10
41
29
5
0
0
0
5
H. campanul atum
10
280
71
89
0
15
0.
5 88
H. anceps
4
448
115
111
0
470
23
111
Planorbula armigera
0
560
147
67
0
480
49
67
P. campestris
148
280
210
6
0
13
3
6
Promenetus exacuous
4
654
153
60
0
480
45
59
P. umbilicatellus
12
266
107
6
0
22
4
6
Armiger crista
80
448
241
10
0
480
146
10
Gyraulus parvus
0
654
134
174
0
592
28
174
G. circumstriatus
25
800
222
26
0
602
46
26
G. deflectus
20
800
99
47
0
394
13
46
TOTAL SITES
0
800
122
440
0
1234
24.4
440
All species (except Stagnicola caperata) were
observed in the absence of measurable sulphate
(Table 6), but, as for chloride, only Sttignicota
paliiHtris, Fossaria modicella and Physa. jen-
nessi were found throughout the entire range
sampled. Valvata. sincera. Stagnicola reflexa,
Fossaria decampi and Bulimnea megasoma ap-
peared to be relatively intolerant of sulphate.
For nitrate and nitrite (Table 6), Cincinnatia
cincinnatiensis, Planorbula armigera and Stag-
nicola palustris occurred throughout all or most
of the range sampled. Narrow ranges towards
the lower end of the scale were seen for
Stagnicola re.jlexa. and Marstonia decepta.
Eleven species were observed to tolerate the
highest phosphorus levels (Table 7). Bulimnea
megasoma and Stagnicola rcjlexa appeared to
favor low phosphorus concentrations.
li
Discussion
the study area only niarginallv more
species were found in lakes than in ponds.
Although none of the species appeared to be
restricted to either lakes or ponds, many
Vol. 100(2)
April 30, 1986
THE NAUTILUS 63
TABLE (). Miiiinuiiii, niaxiiiiuni .uid mean values fur sulphate and nitrate/nilrile for t;astrn|ioils in
the study area.
Species
Sulphate, mg/l
Min. Max. x
Mi trate/nitri te, mg/l
N Min. Max. x N
Campeloma decisum
0
0
0
3
0
0.7
3
Valvata sincera
0
2
0.
5 7
1.0
3.3
1.6
6
V. tricarinata
0
170
51
54
0
2.4
1.3
48
Cincinnatia c i nci nnat lensis
0
170
21
25
0
7.5
1.1
25
Marstonia decepta
0
109
13
9
0
1.5
0.8
9
Probythinel la lacustris
0
170
69
6
0
1.2
0.5
5
Amnicola limosa
0
170
23
85
0
2.7
0.9
78
A. walkeri
0
15
4
5
0
1.5
0.9
5
Lymnaea staqnalis
0
334
28
263
0
5.5
1.2
258
Acella haldemani
0
0
0
3
0.8
1.0
0.9
3
Bulimnea megasoma
0
15
3
30
0
5.3
0.7
28
Stagnicola palustns
0
3403
65
182
0
7.2
1.6
174
S. catascopium
0
113
32
12
0.1
1.7
1.1
12
S. caperata
1.6
157
61
3
1.0
2.3
1.5
3
S. reflexa
0
10
2
7
0
1.4
0.5
7
Fossaria dalli
0
39
13
3
0.8
1.3
1.1
3
F. decampi
0
14
4
6
0
2.4
1.2
6
F. exigua
0
161
29
14
0.2
3.3
1.0
14
F. modicella
0
3403
129
49
0
5.6
1.6
49
F. parva
0
148
37
4
0.2
2.4
1.1
4
Physa qyrina
0
334
24
271
0
5.5
1.1
265
P. jennessi
0
3403
190
28
0
6.8
2.2
28
Aplexa hypnorum
0
165
32
37
0
2.4
1.3
35
Ferrissia paral lela
0
104
42
3
0.9
1.5
1.2
2
F. ri vulari s
0
161
18
36
0
5.3
0.6
36
Helisoma trivolvis
0
443
38
204
0
5.2
1.3
197
H. pilsbryi i nf racari natum
0
64
5
15
0
2.8
0.7
15
H. corpulentum
0
5
2
5
0.1
1.4
0.6
5
H. campanul atum
0
108
3
92
0
2.4
0.8
90
H. anceps
0
167
18
114
0
5.3
1.1
112
Planorbula armiqera
0
157
25
70
0
7.5
1.3
68
P. campestns
0
115
45
6
0.9
1.6
1.2
6
Promenetus exaciious
0
158
42
64
0
5.2
1.3
59
P. umbi 1 icatel 1 us
0
159
28
6
0.3
2.0
1.2
6
Armiger crista
0
128
63
11
0.1
2.9
1.4
10
Gyraulus parvus
0
170
32
181
0
5.2
1.2
176
G. CT rcumstri atus
0
158
35
26
0.7
6.8
2.0
26
G. deflectus
0
108
8
49
0
5.3
1.2
47
TOTAL SITES
0
3403
31
456
0
7.5
1.1
445
gastropods showed strong tendencies to occui-
in one of tiiese liahitat types. Aho rt al. (19<S1)
oliserved a similar situation in Finland, where
most snails could be found over a wide range of
water body sizes. The majority of the species en-
countered in the present study were quite
plastic in terms of the water body and substrate
type in which they could occur. Such plasticity
would be exjiected to be advantageous in that
the species' potential for colonization of new
haliitats would be enhanced.
Most of the species (excejit perhaps .S/ai/i/zco/f/
reflexa) could function in highly diverse gastro-
pod cnnimunities, but it is not surprising that
many species were found frequently in less
diverse groupings where interspecific competi-
tion would be reduced. Species found often at
low community diversities were capalile of sur-
viving in more extreme habitats where other
species failed. Species with low mean communi-
ty diversity values, such as Stagnirold rejle.nt
and BiiVuitnea tnefid.^oma. could occur in ex-
treme habitats only at the lower end of the scale
for most chemical parameters and their toler-
ance ranges for these parameters were narrow.
On the other hand, species stich as Stniinicula
64 THE NAUTILUS
April 30, 1986
Vol. 100 (2)
TABLE 7. Miniiiuim. maximum and moan values tor
molybdenum reactive phosphorus for gastropods in the
study area.
Species
Molybdenum react
.ive P
, mq/l
Min.
Max.
X
N
Campeloma decisum
0.48
1.6
0.9
3
Valvata sincera
0.23
7.0
2.3
6
V. tricarinata
0
44.0
6.1
47
Cinclnnatia cinci nnatiensis
0
14.9
2.9
23
Marstonia decepta
0
5.6
3.2
9
Probythinel la lacustris
1.7
15.0
7.1
5
Amnicola limosa
0
44.0
4.1
78
A. walkeri
0
3.6
1.6
6
Lymnaea staqnalis
0
44.0
3.4
258
Acella haldemam
0.60
6.3
3.5
3
Bulimnea meqasoma
0
2.3
0.7
27
Stagnlcola palustris
0
44.0
4.4
174
S. catascopium
0.45
15.0
3.3
12
S. caperata
0.51
3.2
2.3
3
S. reflexa
0
2.4
0.7
7
Fossaria daUi
0.74
5.0
2.3
3
F. decampi
0.56
15.0
4.7
6
F. exiqua
0.04
5.5
1.3
14
F. modicella
0
44.0
6.5
49
F. parva
0
3.1
1.1
4
Physa qyrina
0
44.0
3.4
265
P. jennessi
0
15.7
3.4
28
Aplexa hypnorum
0.04
21.3
6.1
35
Ferrissia parallela
0.62
1.6
1. 1
2
F. rivularis
0
15.7
2.4
35
Hel Tsoma tn vol vis
0
44.0
3.6
197
H. pilsbryi inf racarinatum
0.04
5.6
1.1
15
H. corpulentum
0.46
1.8
0.9
5
H. campanulatum
0
10.6
2.2
90
H. anceps
0
21.3
2.5
112
Planorbula armiqera
0.21
44.0
5.1
68
P. campestris
4.0
12.4
7.0
6
Promenetus exacuous
0
44.0
5.1
59
P. umbi 1 icatel lus
0.35
8.3
3.9
6
Armiqer crista
0.62
44.0
15.7
10
Gyraulus parvus
0
44.0
3.6
176
G. circumstriatus
0.14
12.4
3.0
26
G. deflectus
0
10.6
2.6
46
TOTAL SITES
0
44.0
2.2
445
paluHtrin, Fhysd jniHf'ss), Hciisiinid fricoh'is, IL
anceps, Lyrrmaea stagnnlh and Fen-tssln
nvularis could occur at very wide ranges of
some or all of the parameters examined. Some
of the species in the latter s^rouji were also very
common in the study area, suj^gestinj^ that, in
conjunction with their ability to tolerate a wide
range of conditions, they may also l)e effective
colonizers of new habitats.
A low value for macrophyte community divei'-
sity may be indicative of extreme habitat condi-
tions and/or of new habitats in which succession
has not peaked. BuHnnwd incfidsonui. which
showed a low gastropod and high macrophyte
community diversity, was characteristic of
habitats in the eastern portion of the study area,
where water parameter values may be extreme-
ly low but plant diversities are high because of
the large nutiibers of macrophyte species which
occur in the Precambrian Shield region (Pip,
1979, 1984). Low diversity values for both
gastropods and macrophytes, as seen for Phym
jennessi. Fossaria exigua and Stagnicola
palustris. probably reflected not only extreme
habitat conditions, but also the pond water body
ty])e which was predominant for these species.
Macrophyte diversity is characteristically low in
ponds. Some regional differences in both gastro-
pod and macrophyte community diversities ap-
pear to exist for a given snail species (Pip, 1985).
The species present in the study area formed a
continuum with respect to the habitat types in
which they were found. At one end of this con-
tinuum could be placed Stagnicola palustris,
Physa jennessi and Fossaria modicella. These
species frequented ponds and a clay substrate.
The variability of water quality in such habitats
was associated with very wide tolerance ranges
of these species for pH, total dissolved solids,
total alkalinity, chloride and sulphate.
At the other end of the scale were Stagnicola
rejlexa, Bulimnea ynegasorna, and, to a lesser ex-
tent, Marstonia decepta. The first two species
were found most frequently in lotic habitats,
while the last species was found in lakes. All
were found primarily in Precambrian Shield
habitats and were characterized by narrow
tolerance ranges at the lower end of the scale
for total dissolved solids, total alkalinity,
chloride, sulphate, nitrate and nitrite and
phosphorus. Mean parameter values were also
low for Helisoma campanulatum, although this
species could tolerate somewhat broader ranges
for some parameters than could the latter three
species, and possible because of this reason it
was the commonest of this group. These species
may be regarded as oligotrophic/dystrophic
specialists.
In general, species which could tolerate high
water chemistry parameter values tended to
have wide tolerance ranges. Although species
with wide tolerance ranges coulcl survive in
hal)itats with lower parameter values, they fre-
(luenled sites with higher levels of dissolved in-
organics, as seen from tlu'ir mean values.
Species such as .Arniiger crista. Physa jcinn'ssi
and Fossaria modicella show high mean values
for total dissolved solids and this may be one
reason why these species are extremely rare
east of the Precaml)rian Shield boundary, where
Vol. 100(2)
April 30, 1986
THE NAUTILUS 65
water parameter values are low. Plnn(irl}itla
campestris may also belong to this group but
was insufficiently sampled in the present study.
A number of workers (e.g. Aho, 1966, 1978;
Dussart, 1976; Okland, 1979; Pip, 1978; Dillon
and Benfield, 1982) have found that calcium
hardness, total alkalinity and pH are important
factors in determining the distribution patterns
of many freshwater gastropods. Okland and
Okland (1980) found that few gastropods occur-
red below pH 6.0 in Norway, with only a few
species, not stated, being able to tolerate values
as low as 5.2 (Okland, 1979). Aho (1978) ob-
served that fewer species occurred at lower than
higher pH values in Finland. The findings of the
present study supported this observation up to
moderately alkaline values. However in the
study area five species could occur at pH values
as low as 5.0. Mackie and Flippance (1983) found
that in southern Ontario Heli><oma anceps and
Amnicola limosa could occur at pH 5.5; this
record for the latter species was lower than the
minimum of 6.1 seen in the present study. The
latter workers also reported a minimum of 6.0
for Cincinnatia cincinnatiensis and \'nlvata
tricarinata. compared to 7.3 and 6.7 respective-
ly in the present study. Ranges for all other
gastropods reported by these workers fell
within the ranges obtained in the present study.
Mackie and Flippance (1983) also found a
lower total alkalinity level of 5 mg/l CaCOj for
C. cincinn.atieniiis compared to a value of 14 in
the present study. All other ranges found by the
latter workers were within those given here.
The tolerance range of a given gastropod
species for a particular parameter must be
viewed in the context of the geographical area
where it occurs. Aho (1966, 1978) found that
with respect to pH and calcium content, snail
species in Finland appeared to occur in lakes
with lower values for these parameters than in
Sweden or Britain. Similarly Pip (1985)
reported that populations in Precambrian Shield
waters often seemed to tolerate lower values of
dissolved inorganics than did populations to the
west of the Shield boundary. Apparently many
species may undergo adaptation according to
the water cjuality characteristics predominant in
the region.
The gastropod communities found in Precam-
brian Shield waters in the study area appear to
tolerate lower minimum pH values than the
communities reported by Okland (1979) in
Norwegian lakes. Perhaps this difference is
related to the type and duration of acid condi-
tions in the two areas. The acidity of undis-
turbed Precambrian Shield lakes is derived
largely from dissolved organic matter; sulphates
are typically absent. The acidity of the lakes
studied by Okland (1979) is a comparatively re-
cent development as a result of acid precipita-
tion. Thus snails in the former case have had
more opportunity to adapt and the acidity is of
different chemical origin. Okland (1979) sug-
gested that the importance of a given water
ciuality parameter such as pH may be related to
the level of other factors present. For example
Pip (1985) found that the relative importance of
specific factors may change in different geo-
graphical regions. Thus the tolerance range for
a particular parameter may be a complex func-
tion of genetic and physiological traits combined
with the relationships between different
chemical entities in the water itself. It is also
possible that additional habitat characteristics,
such as substrate and the kinds of other
organisms present in the community, for exam-
ple vegetation, may further mitigate or ag-
gravate the response of a given snail population
to a specific parameter. A better understanding
of the factors which affect snail distribution in a
given area can only be achieved when compar-
able data becomes available for a number of
geographical regions.
LITERATURE CITED
Alio, .1. 1966. Ecological liasis of the distribution of the
littoral freshwater molluscs in the vicinity of Tampere,
South Finland. Arm. Zool. Ferin. 3:287-322.
1978. Regional variation in the diversity of fre.sh-
water gastropods in southern an<i western Finland. Puhl.
Utiif. Joen.'iiiu. Ser. B, No. 8, 10 pp.
Aho. .J., E. Ranta and J. Vuorinen. 1981. Species composi-
tion of freshwater snail communities in lakes of southern
and western Finland. ylwH. Znnt. Ferin. 18:233-241.
Clarke, A. H., .Jr. 1973. The freshwater molluscs of the
Canadian Interior Basin. Mnlacologia 13:1-509.
1981. The Freshwater MoUusrs of Cnnndii.
National Museums of Canada, Ottawa. 446 pp.
Dillon, R. T. and E. F. Benfield. 1982. Distribution of pul-
nionate snails in the New River of Virginia and North
Carolina, U.S.A.: interaction between alkalinity and
stream drainage area. Fre^hunter Biol. 12:179-186.
Dussart, G. B. J. 1976. The ecologj' of freshwater molluscs
in north west England in relation to water chemistry.
J,,iir. moll. Sli«li,:'< 42:181-198.
Harman, W. N. and C. 0. Berg. 1971. The freshwater snails
66 THE NAUTILUS
April :W. 1986
Vol. 100(2)
of central New York wiUi illusli-atfd keys tci the n*'ii''''<i
and species. Si'inrh: Curnell I'niv. Ani'ic. Kx|i. Station
1:1 -OS.
Macan, T. T. 1 ;».')(>. F^colnKX <>t' freshwater Molhisca in the
Engiish Lake District. ./..»/•. Anini. EciA. 19:124-146.
19.')7. Chemical analysis in ecokigj' illustrateii
front Lake District tarns ami lakes. 3. Faunistic differ-
ences. Priir. Lnm. Sm- Lniiilmi 167: 172-I7"i.
Mackie, G. L. and L. A. Khppance. 1983. Intra- and inter-
specific variations in calcium content of freshwater mol-
lusca in relation to calcium content of the water. Jitiir.
imill. &7h(//>.s' 49:204-212.
Okland. J. 1979. Distriliution of environmental factors and
fresh-water snails ((lastropoda) in Norway: use of Rum-
pean invertebrate survey principles. Muliu-olnijii: 18:
211-222.
Okland, .1. and K. A. Okland. 19,S(l. pH level and food
organisms for fish ■ studies of UKK) lakes in Norway. In
Proc. Internat. Conference on the ecological im|:iact of
acid precipitation. Norway. 1980 (D. Drablos and \.
Tollan, eds.). SNSF Project, pp. 326-327.
Pip, E. 1978. A survey of the ecology and composition of
submerged aquatic snail-plant ciminiunities. Cniuididn
■Inn,-. Zoi.l. 56:22(;.3-2279.
1979. Survey of tlie ecology of submerged
aquatic macro|ihytes in central Canada. AijikiHc Hatdiiy
7:339-357.
1984. Ecogeographical tolerance range variation
in ai|uatic macrophytes. Hydrobidloyid 108:37-48.
1985. The ecology of freshwater gastropods on
the southwestern edge of the Precambrian Shield.
Cariddinri Fii'hl-Nitt. 99:76-85.
PSEUDOSUCCINEA COLUMELLA (LYMNAEIDAE) IN THE DOMINICAN
REPUBLIC AND TRANSMISSION OF
FASCIOLIASIS IN THE CARIBBEAN REGION
Jose Gomez, Mercedes Vargas
Departanieiitd dv Micrdhioiogia y Parasitologia
Universidad Autonoma de Santo Domingo
Dominican Reiuihlic
and Emile A. Malek
Depaftment of Tropical Medicine
Tulane University
New Orleans 70112-2699
ABSTRACT
Pseudosuccinea columella (Sai/. 1817) is reported for the first time from the
Dominican Republic and from the island of Hispaniola. It occurs together with
Fossaria cuhensis (Pfeiffer, 1839) in Puerto Rico, Cuba. Jamaica, and Venezuela
in addition to the Dominican Republic in the Caribbean region. The two lymnaeid
species can be differentiated by shell and animal characteristics. FascioiiasiH is
transmitted in this region p7-incipaUy by F. cubensis, but the occurrence of P. col-
umella in some countries and it.^ jtrobaJite introduction into others may e.rlend the
range of this disease.
Pseudosuccinea columella (also referred to as
Lymnaea columella and Lymnaea (Pseudosuc-
cinea) columella), a North, Uentrtd and South
American species, has a[)parenUy been intro-
duced into certain islands of the Caribbean and
in other regions such as Europe, Africa,
Australia and New Zealand. Maiek and
Chrosciechowski (1964) iind Malek and Cogswell
(1980) reported its occurrence in Venezuela,
Colombia, Costa Rica, Pantima and Brazil and
reviewed its geogrtiphical distribution.
F'araense (1982) also outlined its distribution in
the neotropical region.
In our freshwater snail survey in the
Dominican Re{)ublic we encountered P. col-
umella, but it was less common (3 localities)
than the other lymnaeid, Fossaria cubensis
(Pfeiffer, 1839) (28 localities). Previous reports
of the molluscan fauna of the Dominican
Republic did not include P. columella (see
Crosse, 1891), nor did Alvarez and Cordero
(1977) in their work on fascioliasis report P. col-
umella; they only discussed F. cubensis.
The two lymnaeid species can be differen-
tiated morphologically as follows: The shell of P.
columella has a low spire, much shorter than the
Vol. 100(2)
April 30, 1986
THE NAUTILUS «7
high and elongated aperture, with a large and
expanded body whorl. The surface is sculptured
with microscopic raised spiral periostracal
threads. Lateral teeth of the radula are tri-
cuspid. The penis sheath is short, less than half
the length of the prej)utium. The prostate is long
and narrowly, roundly cylindrical, with the
proximal end somewhat enlarged. P. rohonella
is aquatic, with a tendency to be amphibious.
The adult shell of Fossarm cubensis is small,
with well-impressed sutures and usually in-
distinct spiral lines. The spire is conic, broadly
pyramidal or acute, the aperture is much
smaller when compared to that of P. columella.
The columella is smooth; the inner lip of the
aperture is folded backward, forming a
moderate or broad flat expansion. The lateral
teeth of the radula are bicuspid. The penis
sheath is two-thirds the length of the preputium;
the prostate is ovate and rounded at the ex-
tremities. F. eubensis is amphibious.
Reports of P. colitmelht in addition to F.
cubensis from other Caribbean islands are from
Puerto Rico (van der Schalie, 1948; Harry and
Hubendick, 1964; Leon-Dancel, 1970) and from
Cuba (Aguayo and Jaume, 1949). Specimens
received from Ms. Charmine Crawford from
Jamaica are also P. columella and F. cubensis.
The two species are also known to occur in
Venezuela (Malek and Chrosciechowski, 1964).
P. columella, has not been reported from St.
Lucia (Malek, 1965; Barnish el ai. 1980),
Guadeloupe (Pointier, 1974, 1976), Martiniciue
(Guyard and Pointier, 1979), or Haiti (Robart et
ai. 1976); however, F. cubensis is present in
these countries. Pilsbry (1910) described the
subspecies F. citbensis aspiraus as Liitunaea
cubensis aspirans from Barbados, West Indies.
The liver tluke Fasciola hepatica. which
causes fascioliasis in the Americas, occurs in
cattle and sheep-raising countries, parasitizing
these animals and other herbivores. Human
fascioliasis has also been reported from alnwst
every American country, including islands of
the Caribbean. There are several early reports
of high prevalence rates on Cuba and records of
some human cases. There are also records of
fascioliasis in the Dominican Republic (Ueno et
ai, 1973; Alvarez and Cordero, 1977), Puerto
Rico (Frame and Bendezu, 1978; Hillyer, 1981;
Bendezu et a I.. 1982), Martinique (Gretillat,
1966, 1967), St. Lucia (Malek, 1965, 1980;
Barnish et ai. 1980), and .Jamaica (Anonymous,
1960). Malek (1965) signaled the occurrence of
fascioliasis in St. Lucia and later (1980) gave
details of prevalence rates in several estates in
the north, center and south and in the abattoir
in Castries, the capital. Malek (1965) predicted
the occurrence of lymnaeid snails on the island
and shortly after the report was written F.
cubensis was encountered in 4 localities. The
snails from St. Lucia were infected exjierimen-
tally with F. hepatica miracidia of St. Lucian
origin, and were later photographed (Malek,
1980). F. cubensis from St. Lucia was also
susceptible to the schistosome, Heterobilharzia
aniericana (Malek, 1967).
From all reports it seems that in the Carib-
bean region the principal snail intermediate host
of F. hepatica is F. cubensis. P. columella,
although susceptible to experimental infection
(Leon-Dancel, 1970), has not been found
naturally infected where it occurs in the Carib-
bean region, although natural infection has been
reported in Brazil (Ueta, 1980). There is also a
record by Van Volkenberg (1939) (cited in Leon-
Dancel, 1970) and one by Hillyer (1981) in which
P. cdhanella was stated to be an intermediate
host in Puerto Rico. The natural and experimen-
tal infections in P. columella indicate that its
presence in some Caribbean countries, and its
likely introduction in others, may extend the
range of fascioliasis in the region.
References in the literature suggesting that
snails other than lymnaeids, for example Pliysa
cuboixis in Cuba or terrestrial snails, can act as
intermediate hosts for F. hepatica are er-
roneous. Some authors tend to implicate snails
other than lymnaeids as transmitters of
fascioliasis when they fail to locate lymnaeids
such as F. cubensis or P. cnhouclla in the Carib-
bean region. Moreover, Leon-Dancel et al.
(1971) tested the susceptibility of Physa cubensis
and Aple.ra marmorata in Puerto Rico and
found them refractory to infection with F.
hejiatica.
LITERATURE CITED
Atrunv". ('. ('.. anil .lauriie. M. L. U)41). Faniilia Lyninaeidae.
(in i:i47-l'.l.'>:i) ' 'atiihyi, ili /.,s Molliisms ,!>■ Ciiha, No. 4;t,
Ciilia.
68 THE NAUTILUS
April 30, 1986
Vol. 100(2)
Alvarez. .1. M. V. and Conlcro. E. T. C. 1977. Fasciolosis
bovina en la Republica Domiiiioana. PuU. Universidad
Aulonoma S. Domingo, Vol. 224, Col. Cienciay Techti. No.
5:1-189.
Anonymous. 1960. Annual report Ministry Agriculture
.lanuiica, 31 December I9.')8.
Barnish, 0.. Prentice, M. A. and Harris. S. 1980. Fasciola
h<'i>(ittc<i in St. Lucia, West Indies. British Vet. Jour.
136:299-300.
Bendezu, P., Frame. A. and Hillyer, G. V. 1982. Human
fascioliasis in t'onrzal, Puerto Rico. Jour. Pnnisitol.
68:297-299.
Crosse, H. 1891. Faune malacologique terrestre et tluviatile
de I'ile de Saint Domingue. Jour. Conrhyiiol. 39:69-211.
Frame, A., and Bendezu, P. 1978. Bovine fascioliasis in
Puerto Rico. Jour. Parasitol. 64:136.
Gretillat, 8. 1966. Lymnaen cuhensif! Pfeiffcr 1911, niol-
lusque bote intermediaire Ae Fnsrioh Iwpatirn L., 1758 a
la Martinique. C. R. Acad. Sri. Pnris 262:2736-2739.
1967. Prospection malacologique aux Antilles
Francaises. Observations sur I'ecologie et I'elevage au
laboratoire de Lymnapn ruben.sis. Ren Elev. Med. Veter.
Poys Trop. 2:279-289.
Ciuyard, A. and Pointier, .1. I\ 1979. F^aune malacologique
<luIcaquicole et vecteurs de la schistosomose intestinale en
Martinii(ue (Antilles Francaises). Arm. Pitrnsitol. (Paris)
54:193-20.5.
Harry, H. W. and Hubendick. B. 1964. Tlie freshwater pul-
monale mollusca of Puerto Rico, Med. Ootehorys Mii.'i.
Zooi Ard. 136:1-77.
Hillyer, (!. V. 1981. Fascioliasis in Puerto Rico. [A review.]
Bol. A HOC. Med. Puerto Rico 73:94-101.
Leon-Dancel. D. 1970. Life history of Lymnaeo i-otioiielln
(Say) and its experimental infection with Fri.sr/o/d hepotico
(L.). Jour. Agric. Unir. Puerto Rieo 54:297-30.5.
Ritchie, L., and Chiriboga. .1. 1971. Refractive-
ness of P/ij/.S(( ruherma (Pfeiffer) and .Aple.rn mormorntn
(Guilding) to Fa.friota hepotico (L.). Jour. .Agric. Unir.
Puerto Rico 55:267-270.
Malek. F>. A. 1965. Freshwater and land snails of St. Lucia,
the West Indies. Arner. Malncol. Union. Annual Reports,
p. 38.
1967. E^xperiniental infection of several lym-
naeid snails with Hetero))ithnrzi(i nmi'ricono. Jour.
Pariiiiitol. 53:700-702.
1980. Snail Trnnaniitted Paraaitic Diseases,
Vol. n, CRC Press, Boca Raton, Florida. 324 pp.
and Chroscieehowski, P. 1964. Lymnaea (Pseu-
dosuccinea) columella from Venezuela, and notes on distri-
bution <){ P.'ieudosuecinea. The Nautilus 78:54-56.
and Cogswell, F. B. 1980. Lymnaea (Pseudosuc.-
cinea) columella in Colombia. The Nautilus 94:112-114.
Paraense, W. L. 1982. Lymnaea riatrix and Lymnaea col-
umella in the Neotropical region: A distributional outline.
Mem. Inst. Clswaldo Cruz 77:181-188.
Pilsbry, H. A. 1910. Lymnaea cubensis nspirans n. subsp.
The Nautilus 23:\2{)'.
Pointier, .1. P. 1974. F^iune malacologique dulcaquicole de
I'ile de la (Hiadeloupe (Antilles Francaises). Bull. Mus.
Hist. Natur.. Paris, 3rd Ser., No. 235, Zool., 1.59:905-933.
1976. Repartition locale el biogeographie des
mollusques dulcaquicoles de la Guadeloupe (Antilles
Francai.ses). Malacol. /?e<'i>H' 9:85-103.
Robart, G.. Mandahl-Barth. G. and Ripert. C. 1976. Inven-
taire, repartition geographique et ecologie iles mollusques
dulcaquicoles d'Haiti (Caraibes). Haliotis 8:159-171.
Heno, H.. Alvarez. .J. M. V., Mergen. A. M. R. de and
Sanchez, V. M. 1973. Observation on the prevalence of
parasitic diseases in cattle especially fascioliasis, in the
Dominican Republic. Nat. Inst. Animal Hlth. Quarterly
(Tokyo) 13:59-68.
Ueta, M. T. 1980. Ocorrencia de infecvao natural dv Faxciola
hepatica Linnaeus. 1758 em Lymnaea columella Say. 1817
no Vale do Paraiba. SP. Brasil. Rec. Saude Publico 14:
230-233.
van der Schalie. H. 194cS. The land and fresh water niollusks
of Puerto Rico. Misc. Publ. Mus. Zool. Univ. Michigan,
No. 70.
ANNOUNCING THE CO. A.
19S6 CONVENTION
The Concholo^ists of America's 14th annual
convention will he held at the Sheraton \'ankt'e
Trader Hotel at Fort I Lauderdale, Florida, from
July 1') throujjjh July 19, 198(5. The convention
will he hosted hy the Broward Shell Cluh, and
the CO. A. welcomes all shell collectors,
whether novice or advanced, as well as shell
dealers and scientists from aroinid the country
and the world.
For further information and pre-registration
packets, please contact Ruth ('hesler. Conven-
tion Chairman, at 7401 S. W. 7th Street. Planta-
tion, Florida 8:5317.
NEWS
JULY 1986 AMU MEETING
The American Malacological Union and the
Western Society of Malacolojjists will have a
joint meetin,ti; from July 1-5 at the Sheraton
Hotel in the heart of historical Monterey, Calif.
The three symposia will be on the biolojjy of
opisthohranchs, life history of cephalopods and
molluscan morphological analyses. Housing,
travel and registration details, already sent to
AMU members, may also be obtained from
President Dr. James Nybakken, Marine Labora-
tories. P.O. Box 450, Moss Landing, CA
95039-0450.
Vol. 100(2) April ::5(), 1986 THE NAUTILUS 69
SOME ASPECTS OF THE EVOLUTION OF THE RUDIST PELECYPODS
David Nicol
Box 14376, University Station
Gainesville, FL 32604
ABSTRACT
The evolution of the rudist pelecypods was remarkably rapid even as compared
to many mammalian groups. One new genus appeared every 1.900,000 years in
the Late Jurassic, hi the Early Cretaceous, one neiv genus appeared every
1,370,000 years, hut iii the Late Cretaceous the rate of evolution accelerated great-
ly when one new genus appeared every 3^5,000 years. For the entire time-span for
the existence of the rudists, one new genus appeared every 738,000 years. Like the
dinosaurs, the first rudists were of modest size. Beginning in the AUiian stage,
some rudists attained a size as large as any pelecypods that have ever lived.
Some additional aspects of the evolution of the
rudists are given here because they are either
not mentioned or inadequately covered in a
manuscript now in press (D. S. Jones and D.
Nicol: Origination, survivorship, and extinction
of rudist taxa). Some of the data used herein
were updated by examining the Zoological
Record from 1966 to 1981. The main source of
data is the Treatise on Invertebrate Paleon-
tology (C. Dechaseaux and A. H. Coogan, 1969).
The aspect that is particularly emphasized
here is the rapid increase in diversity at the
generic level, especially during the Late
Cretaceous or the last 29 million years of the ex-
istence of the rudists. The 15 Jurassic and
Cretaceous stages listed in Table 1 are based
primarily on ammonite zones and are not all of
the same duration. The duration in years of each
stage was taken from Palmer, 1983. The 15
stages can be subdivided into three groups for
studying the changes of rates of evolution: the
three Jurassic stages (Oxfordian through Titho-
nian), the Early Cretaceous stages (Berriasian
through Albian), and the Late Cretaceous
stages (Cenomanian through Maastrichtian).
Rudist evolution began at a rather modest
rate in the Late Jurassic with a new genus ap-
pearing approximately every 1,900,000 years.
The evolutionary rate did not accelerate greatly
during Early Cretaceous time when a new
genus appeared every 1,370,000 years. How-
ever, beginning with the Cenomanian, the
earliest stage of the Late Cretaceous, evolution
speeded up greatly, and a new genus arrived
every 345,000 years. The evolutionary rate for
TABLE 1. The I.t Jurassic and Cretaceous stages with
their duration in millions of years, number of new genera per
stage, and new genera per year. Oxfordian -Tithonian. Late
Jurassic; Berriasian -Albian, Early Cretaceous; Ceno-
manian- Maastrichtian, Late Cretaceous.
stages
Duration
Mew
:e^ £-n-rd
in years
jenera
per ye^r
■■■'aastrichtia.a
",000,000
17
470,000
Campanian
9,500,000
13
730,000
Santonian
2,500,000
15
100,000
Coniacian
1,000,000
10
100,000
Turonian
2,500,000
13
192,000
Cenomanian
5,500,000
lo
344,000
Albian
15,500,000
10
1
, 55o,000
Aptian
0,000,000
7
"57,000
Barresnian
5,000,000
9
025,000
Hauterivian
7,000,000
0
— 0—
Valanginian
7,000,000
5
1
,400,000
rerriasian
0,000,000
4
1
,500,000
Tithonian
8,000,000
4
2
,000,000
Kimmeridgian
4,000,000
0
— 0—
Oxfordian
7,000,000
0
1
,107,000
Totals
94,500,000
12'!
73 ",000
the total 15 stages, or the complete life span of
the rudists, is the appearance of a new genus
every 738,000 years. This would be considered
exceedingly rapid evolution amongst the pelecy-
pods in a stable marine environment and is com-
parable to rapid evolutionary rates in many
THE NAUTILUS
April ;i(), 1986
Vol. 100(2)
groups of mammals.
The rapid acceleration of evolution of the
rudists during the Late Cretaceous appears to
be based on two phenomena. First, the three
larger and more rapidly evolving families
(Caprinidae, Radiolitidae, and Hippuritidae)
either did not appear until the Late Cretaceous
or did not become diverse until that time. Sec-
ond, the rudist faunas became more provincial
and ecologically complex in the Late Cretace-
ous. Endemism of the rudist genera increased
greatly in the Late Cretaceous, and the rudist
communities were generically most diverse in
the Caribbean region during the Maastrichtian
(Kauffman and Sohl, 1974).
As more paleontological study is done in the
more remote areas with Jurassic and Cretace-
ous rocks in the Tethyan realm, a greater
number of new genera discovered will be in the
Late Cretaceous rather than in the Early
Cretaceous and Late Jurassic.
In the rates of evolution within the L5 stages
in Table 1, it is worthwhile to point out a few
additional features. After a good start in the Ox-
fordian Jurassic, the evolution of the rudists
slowed somewhat with a gap of no new genera
in the Kimmeridgian, a time span of four million
years. This slowing of the rate of evolution con-
tinued into the first three stages of the Early
Cretaceous with a climax in the Hauterivian
when, again, no new genera have so far been
discovered. The unusual aspect of the Hauteri-
vian gap is that it encompassed approximately
seven million years.
Beginning in the Barremian, evolution accel-
erated greatly and this may have been caused
partially by the onset of the two most diverse
families, the Caprinidae and Radiolitidae. The
rate of evolution then slowed in the next two
stages which end in Early Cretaceous times.
New genera appeared with exceeding rapidity
in the Cenomanian and continued unabated until
the Campanian and then accelerated again in
the Maastrichtian. In the latest Cretaceous, new
rudist genera were still appearing at a very
rapid rate.
Although extinction of genera occurred rapid-
ly in the Late Cretaceous, the large number of
new genera in each stage tended, with some ex-
ceptions, to increase the total number of genera
in each stage to a maximum of 43 in the
Maastrichtian. This total of 43 includes the
holdovers from earlier stages as well as the new
arrivals. The present total of rudist genera is
128 so that within a period of no more than eight
million years, one third of all the rudist genera
became extinct. Five of the seven rudist families
also became extinct in the Maastrichtian.
The decline and extinction of the rudists oc-
curred in slightly less than 8.5% of their total
geologic history. This sudden demise of the
rudists at their zenith at the end of the
Cretaceous is unlike the extinctions of the
trilobites, graptolites, conodonts, and rostro-
conchs where there was a long period of decline
in diversity before extinction. Even the am-
monites and dinosaurs experienced a longer
period of decline than the rudists. It is most dif-
ficult and highly speculative to explain such a
sudden extinction in a group of marine pelecy-
pods that had been so highly successful.
The rudist pelecypods, like the dinosaurs,
began with small-sized species. Some of the
early rudists were about 20 mm long, and small-
sized rudists are also found at the end of the
Cretaceous in Maastrichtian strata. Particularly
among the diverse families Caprinidae and
Radiolitidae, some stocks attained large size as
early as the Albian, and large species continued
to occur into the Maastrichtian. However, even
by Albian time, 50 million years had passed,
which is more than half of the total time span of
the rudists. Titanosarcolites attained a length of
more than 2 m, Bournonia reached a diameter
of more than 0.6 m, and the shell wall of
Durania attained a thickness of at least 10 cm
(B. F. Perkins, 1969, p. N751). These large
rudists were among the largest pelecypods that
have ever lived.
Acknowledgments
I am indebted to Gary S. Morgan of the
Florida State Museum for making some helpful
suggestions that improved this paper.
LITERATURE CITED
Ilechaseaux. ('., and A. H. Coogan. 1969. Hippuritacca-
Systeniatic descriptions, p. N776-817. In R. C. Moore (ed.).
Treatise on Invertebrate Paleontology, Part N, Vol. 2,
Mollusca 6, Bivalvia. Univ. Kansas Press, Lawrence.
Jones, D. S., and D. Nicol. Origination, survivorship, and
extinction of rudist taxa. Jour. Paleo. 60:107-115.
Kauffman. E. ti.. and N. F. Sohl. 1974. Structure and evolu-
Vol. 100(2)
April 30, 1986
THE NAUTILUS 71
tion of Antillean Cretaceous rudist frameworks. Verhand-
lungen Naturfor.'ichende Gesellschaft. Basel. 84:399-467.
Palmer, A. R. 198,3. The decade of North American geologT,-
1983 geologic time scale. Geology ll:.503-504.
Perkins. B. F. 1969. Rudist morphology' -Shell size ami
shape, p. N7.")l. In R. C. Moore (ed.). Trcntixc on hirci-tr-
bmte Paleontology, Part N, Vol. 2, Mollusca 6, Bivalvia.
Univ. Kansas Press, Lawrence.
Zoological Record. 1966-1981. The Zoological Society of
London.
A NEW SOMATOGYRUS FROM THE SOUTHWESTERN OZARKS WITH
A BRIEF REVIEW OF THE HYDROBHDAE FROM THE
INTERIOR HIGHLANDS (GASTROPODA: PROSOBRANCHIA)
Mark E. Gordon
Department of Zoology
University of Arkansas
Fayette vi"lle, AR 72701
ABSTRACT
A previously unknown Somatogyrus is described from the Elk River, McDoridld
County, Missouri. With this description, the number of Hydrobiidae presently
recorded from the Interior Highlands increases to 15, including 11 regional
endemics. Nine species are endemic to the Ozark Plateaus, while two
Somatogyrus are restricted to the Ouachita Mountains. Fire of the Ozark
endemics are obligate troglohites. Troglobitic Amnicola antroecetes (Hubrichf) is
considered distinct from epigean A. aldrichi (Call and Beecher).
Excepting the Unionoidea, little study has
been afforded the aquatic Mollusca of the In-
terior Highlands. Among the poorer known
groups, regional accounts of the Hydrobiidae
are rare. The primary sources of pulilished
records have been original descriptions of
several endemic species (e.g. Walker, 1915;
Hinkley, 1915; Hubricht, 1979), although the oc-
casional collection of hydrobiids has been noted
in a few species surveys (e.g. Sampson, 1913;
Wheeler, 1918; Gordon, 1981). A recent faunal
survey of drainage basins in southwestern
Missouri and northwestern Arkansas (Gordon,
1980) recovered several species of Hydrobiidae.
A previously unknown Somatogyrus. collected
from the Elk River, McDonald County,
Missouri, is here described.
Family Hydrobiidae Troschel 1857
Subfamily Lithoglyphinae Fischer 1885
Somatogyrus rosewateri new species
Shell descripfiori of holotype-SheW sub-
globose, medium size for Somatogyrus. solid,
dextral, 4.25 whorls, turbinate, subhyaline; body
whorl .90 times axial height, greatly inflated;
[penultimate whorl .34 times width of body whorl
(Fig. 1; see Table 1 for holotype measurements
and range of paratypes). Spire very short,
depressed, broadly conic; sutures moderately
impressed; protoconch flattened (Fig. 2).
Periostracum greenish (may be masked by color
of visceral mass showing through shell) with
shallow, oblique growth striae; protoconch or-
namented with fine, spiral ridges (Fig. 3). Aper-
ture broadly ovate, .74 times axial height, .80
times height and .55 times width of body whorl,
plane of aperture at 30° to shell axis. Peristome
complete across parietal wall by a callus which
continues and thickens across columella (callus
in some individuals may be slightly reflected
over columella, partially obscuring umbilicus);
lip straight along parietal wall, curving con-
cavely near the umbilicus and along columella,
parietal-columellar junction non-angular. In
lateral view (Fig. 4), periphery of parietal lip
72 THE NAUTILUS
April 30, 1986
Vol. 100 (2)
FIGS. 1-5. Suiniit(i(j!irus nuiruvlcn n. .sp. 1, apei'tural view
(if paratype (3.9 x 3.8 mm.); 2, juvenile paratype; 3, suture
and pr<)t(jconeh sculpture iif paratype. The liarely visible
white bar in the upper left is 10 micrcms in length. 4, lateral
view of paratype (4.2 x 3.8 nun.); 5, urnhilical view (if
paratype (shell, 3.fi x 3.5 mm.).
approximately parallel to plane of aperture, col-
umella straight but recedes towards base, and
parietal-columellar junction forma an obtuse
angle. Umbilicus relativi'ly open for Somnfo-
gyrus (Fig. 5); passes into a shallow, canal-like
depression continguous to the columellar Iif).
Basal lip slightly receded due to angle of aper-
ture; area of base-columcllar junction projects
forward about ecjual to the distance of the basal
lip recession (Fig. 4).
Operculum chitinous, ovate, horn-colored;
paucispiral, consisting of about three whorls;
nucleus subcentral, located slightly left of
midline in lower third; outer surface sculptured
with many fine growth striae, peripheral margin
without striae and edge appears slightly ragged
(Fig. 6).
Soft paW.s- Living animals translucent (odon-
tophore complex visible through proboscis),
whitish. Mantle collar and dorsal aspects of pro-
boscis, head, tentacles, and foot speckled with
sub-epidermal gold to orangish gold chromato-
cytes (Fig. 7); dorsal surface and V3 thickness of
visceral mass infused with golden color. Dense
concentrations of melanin at base of tentacles,
extends dorso-medially in front of eyes a short
distance and posteriorly on to dorsum of head
(Fig. 8); a narrow line of melanin runs laterally
from in front of eye forward about V4 to Vs
length of tentacle; dorsal and lateral surfaces of
mantle with mottled patterns of melanin (Fig.
7), 35% of paratypes (n = 52) lacked mantle
melanin. Shells of living snails appear amber to
orangish due to visceral and mantle pigmenta-
tion showing through shell, darkens to brown in
spire; melanistic snails have slightly browner
tint. Penis unpigmented. Preserved animal
white.
Foot broad (Fig. 7); anterior truncated, ex-
tending forward to eyes; posterior tapers to a
rounded point. Head (Fig. 8) extends anterior of
shell to expose eyes; proboscis relatively long
and slender, curved ventrally; tentacles long
and slender, eyes positioned ventro-laterally at
base. Penis (Fig. 9) slender, simple; tapers to a
fine, blunt point; dorso-ventrally flattened, dor-
sum slightly convex, venter flatly concave; vas
deferens positioned near posterior margin.
Penis arises a short distance inside mantle cavi-
ty above and behind the right tentacle, tends to
curve counter clockwise; when extruded,
emerges from shell directly behind right ten-
tacle and extends below it (Fig. 8).
Type locality -M\ssour\, McDonald County,
Elk River at Missouri Department of Conserva-
tion Mt. Shira Public Fishing Access, 1.6 km
south of Ginger Blue (R33W, T21N, sections 1
and 2). Holotype: University of Colorado
Museum of Zool()g>' (UCM) no. 32812; collected
24 October 1985 by Mark E. Gordon. Allotype:
UCM no. 32813; same data as holotype. Para-
types: ten specimens each deposited at UCM,
U.S. National Museum of Natural History,
Academy of Natural Sciences of Philadelphia,
Vol. 100(2)
A|:)ril 80, 1986
THE NAUTILUS 73
TABLE 1. Dimensions of holotype, allotype, and paratypes oi' SumiifiHii/nis niKPimferi (measurements in mm): H =
height, W= width, BH = body whorl height, PW = penultimate whorl width, A = aperture, AH = aperture height,
AW = aperture width.
H
W
W/H
BH BH/H
W/BH
PW
PW/W
AH
AW AW/AH
Plane of A
Holotype
(9i
J. 9
i.8
.97
3,5
90
1.09
1. 3
.34
2.8
2.1
75
30°
Allotype
(o-)
3.4
3.4
1.00
3.1
91
1.10
1.0
.29
2.5
1.9
76
Paratype
3.7
3.6
.97
3.2
86
1.13
1.2
.33
2.3
2.1
91
„„
4.0
3.7
.93
3.5
88
1.06
1.2
.32
2.7
1.7
63
34°
„„
4.1
3.9
.95
3.6
88
1.08
1.2
.31
2.8
2.4
86
29°
„„
4.0
3.8
.95
3.6
90
1.06
1.1
.29
2.9
2.2
/6
tin
3.9
3.7
.95
3.4
87
1.09
i.2
.32
2.5
2.1
84
34°
II It
3.8
3.8
l.OU
3.1
89
1.12
1.3
.34
2.4
2.1
88
35°
„„
3.8
3.5
.92
3.4
89
1.03
1.3
.3/
2.5
2.1
84
30°
(Fig.
1)
3.9
3.8
.97
3.5
90
1.09
1.1
.29
2.5
2.1
84
30°
(Fig.
3,4)
4.2
3.8
.90
J. 7
88
1.03
1.3
.34
2.8
2.2
79
30°
(Fig.
5)
3.6
3.5
.97
3.3
92
1.06
1.0
.29
2.5
1.9
76
27°
FIGS. 6-9. Somatogyrus rosewateri n. sp. 6, operculum; 7, animal extruded from shell
(composite drawing from live and rela,\ed specimens; body slightly distended from relaxa-
tion with sodium pentobarbital): C = chromatocytes, E = eye, F = foot, M = melanin.
Mm = mantle melanin showing through shell. Mo = mouth, 0 = operculum, P = proboscis,
T = tentacle; 8, dorsal view of head: Pn = penis; 9, penis: V = vas deferens.
Museum of Comparative Zoology, University of
Michigan Museum of Zoology, and FieW
Museum; same data as holotype.
Distribution -Found only in the middle sec-
tion of Elk River (Fig. 10). To date, this species
has been collected from only the type locality
and below an old mill dam at Noel, McDonald
County, Missouri. It was not recovered from
74 THE NAUTILUS
April 30, 1986
Vol. 100(2)
ARIANSAS
FKi. Kl. Distriliution of Siini.atofiyrus riiaeiratcri (sdlid
triangle is the type locality).
areas upstream of the type locality nor the river
channel downstream from the Missouri-
Oklahoma border which has been inundated by a
reservoir on the Neosho River (Grand Lake 0'
the Cherokees). The known range of this species
occurs in the Springfield Plateau region of the
Ozarks.
//rr6;7a/- Specimens were collected at the
type locality from a series of riffles. Substrate
was composed of gravel and cobble-sized
materials (mainly chert). At Noel, habitat was
below the outfall of a small mill dam. Substrates
were primarily stepped and broken bedrock
with some cobble. Gradients at both sites were
fairly high and water quality was quite good
(Table 2).
Efyyuology -Th\i^ s|)ecies is named in memory
of Dr. Joseph Rosewater, late Curator of
Mollusks, U.S. National Museum of Natural
History.
Discussion
The comparative difference between S.
rosewateri and previously described species in
the genus are shown in Table 3.
TABLE 2. Physicd-cheniical nieasurenierits madi
locality. Elk River; 20 November, 1979.
at type
Water temperature
Tiirliiility
Specific coruiuctance
Alkalinity
I'll
Nitrate
Color
15°C
1.6 NTU
2(j0 fjmhos/cm
140 mfT/l total CaCUj
8.1.-)
1..') mg/l
neglij^ble
Besides Somatoyyru,^ rosewateri. the only
other hydrobioids collected from the Elk River
basin were the nymphophiline Cincinnatia in-
tegra (Say) and the pomatiopsid Pomatiopsi>i
lapidaria (Say) (Gordon, 1980). Two other
Somatogyrus are known from the Ozark
Plateaux. Somatogyrus depressus (Tryon), an in-
habitant of the upper Mississippi River valley,
occurs in the Osage River, central Missouri
(Thompson, 1984) and S. crassilahris Walker,
an Ozark endemic, is apparently known only
from its original collection from the North Fork
of the White River, Arkansas. In discussing
phylogenetic relationships among North Ameri-
can Lithoglyphinae, Thompson (1984) noted dif-
ficulties in pursuing such studies due to a
relatively large number of undescribed species
and a paucity of morphological data for de-
scribed species. For Somatogyrus. he did list
several characters useful for specific com-
parisons. Available data for the three Ozark
species and two Ouachita Mountains endemics
(Table 3) suggests that the Ozark species may be
fairly closely related. Walker (1915) also con-
sidered S. wheeler i Walker closer to S.
crassilahris than to its Ouachitan congener.
However, both Ouachita Mountains endemics
may have evolved from other lineages (e.g.
Alabama River). Considerably more information
is necessary before such speculative,
phylogenetic relationships may be confirmed. In
some instances, complete analyses may no
longer be possible. Many hydrobiids, such as S.
era.ssilabrls. S. amnicoloides Walker, and S.
wheeleri. are known only from their type
localities. Habitat alterations, such as reservoir
construction, may have been deleterious for
species with such highly restricted distributions.
Fifteen species of Hydrobiidae have been
documented from the Interior Highlands (Table
4). Four are wide-ranging species. In the case of
Prohythvnella lacu.'^tris (Baker) (mistakenly
listed as F. binneyana (Hannibal) in Gordon,
1981) and Somutogyrus depres.'<y.s. their south-
ern distributional limits occur in the Ozarks.
Clncinnaila integra and Birgella subglohosa
(Say) have considerably larger ranges than the
previous, more northerly distributed species
(see Rurch and Tottenham, 1980; Thompson,
1984). The remaining eleven species are
endemic to the Interior Highlands. Somatogyrus
Vol. 100(2)
April 30, 1986
THE NAUTILUS 75
TABLE 3. Variation in shell morpholo^ among Interior Highlands Somalomirti^ (data adapteil
from Baker, 1928; Burch and Tottenham, 1980: Hinkley. 1915; Walker, 191.'); and tliis study).
depress us crassilabris rosewateri wheeleri ainnicoloides
Shell obesity (W/H) .78-1.00
Size
medium {<4 imi)(0) 0
small (> 4 mm) ( 1)
Spire
depressed (>15% H)(0) 0
elevated (<15% H) (1)
Protoconch
flattened (0) 0
elevated (1)
Par ietal-colume liar
wall junction of lip
smooth curve ( 0 ) 0
angular (1)
Umbilicus
narrow { 0 ) 0
open ( 1 )
Widest expansion
of outer lip periphery
above mid-height (0) 0
below mid-height (1)
Aperture apex relation
to parietal wall
fused (0) 0
detached (1)
.77-. 92
.90-1.00
.93
amnicoloides and S. ivheeleri are presently the
only endemic hydrobiids that have been iden-
tified from the Ouachita Mountains province.
Four epigean and five troglobitic species are
endemic to the Ozark Plateaus. The maj(jrity
(eight) are restricted to the eastern half of the
province. The only endemic, western Ozark
hydrobiid presently recognized is S. ro^tewaferi:
however, a single specimen of Somntogyrus has
been collected from the headwaters area of the
White River, Arkansas (Gordon, 1980). This
specimen was too eroded to allow identification
beyond genus and sulisequent collecting failed
to recover additional specimens.
Most of the Ozark endemic, obligate troglobi-
tic Hydrobiidae have been referred to Amnicoli-
nae: Anniicoln. Burch and Tottenham (1980)
noted that this classification was tentative due
to the lack of anatomical flata for these species.
However, Antrobia culreri Hubricht was rele-
gated to the Lithoglyphinae without justifi-
cation by Burch and Tottenham (1980). The
anatomy of this species remains all but
unknown. The brief description of the radula
presented by Hubricht (1971) does not appear to
meet the radular criterion for Lithoglyphinae
established by Thom()son (1984) and differs
from that of Amniroln only by the size of the
central tooth mesocone. Hubricht (1971)
described the penis of Antrohid as "simple,
tapering to a point, without appendages." This
morphology is characteristic of the lithoglyphine
penis (Thompson, 1984) and is prolialily the
basis for the classification in Burch and Totten-
ham (1980). Unfortunately, Hubricht (1971) did
not describe the number of ducts penetrating
the (lenis. Thompson (1984) considered the
Amnicolinae, with two penial ducts, remote in
76 THE NAUTILUS
April 30, 1986
Vol. 100(2)
TABLE 4. Hydrobiidae known from the Interior Highlands.
Hydrobiinae
Prohythinctta iacu.stritt {Baker, 1928)
Lithoglyphinae
Som<itogy7-us amnicoloides Walker, 1915
Su7n.ato(fi/rus crassilabris Walker, 1915
Somntogi/rus depressus (Tryon, 1862)
Somntotfynis rosewateri new species
Somatog-yruit wheeleri Walker, 1915
Nymphophilinae
Birgeila subglohona (Say, 1825)
Cincinnalia Integra (Say, 1821)
Marstonia ozarkensis (Hinkley, 1915)'
Amnicolinae
Amnicolii aid rich i (Call and Beecher, 1886)'
Amnicola antroeretes (Hubricht, 1940)'
Amnicola corae Hubricht, 1979'
Am.nicula prosperpiria Hubricht. 194(1'
Amnicola stygia Hubricht, 197P
Antrolna culvert Hubricht, 197 P
'Pyrgulopsis ozarkertsis is placed in Ma rston ia following the
suggestion of Thompson (1977).
'Burch and Tottenham (1980) included Amnicola mi.s.sowrj-
ensis Pilsbry, 1898 as a valid species. Although this group re-
quires further anatomical investigation, the argument of
Hubricht (1940) for synonymizing this species under .4.
aldrichi is followed.
^Troglobitic.
relationships to the hydrobiid subfamilies
possessing single-duct penes (e.g. Lithoglyphi-
nae). Additionally, Thompson (1984) suggested
that the simple, non-appendaged penis was a
generalized, primitive condition in the
Lithoglyphinae but may occur as a "derived con-
dition through the secondary loss of previously
existing characters" for some taxa in other
hydrobiid subfamilies (e.g. Hershler and Davis,
1980: Hydrobiinae; Hershler, 1985: Littoridini-
nae). Considering similarities of the antrobian
radula, shell, and operculum to Amnicola.
morphology of the penis may represent a
secondarily derived character state mAntmbid.
In conjunction with the above, a conservative
classification would retain A. culveri in the
Amnicolinae until phylogenetic relationships
can be resolved.
The only endemic, epigean aninicoline pre-
sently recognized \?, Amnicola aldrichi (Call and
Beecher), which exhibits a habitat preference
for springs. Hubricht (1940) described three
subsj)ecies ior A. aldrichi: aldrichi s.s., itisolUa
Hubricht, and antroec.ete.a Hubricht. "Deeper
sutures, strongly shouldered whorls, and a free
lip (Hubricht, 1940)" differentiated insolita from
aldrichi s.s. Hubricht's illustration and descrip-
tion of a free lip indicate a slightly uncoiled body
whorl. This condition occurs occasionally within
the Gastropoda and has been shown to some-
times represent distinct, geographical sub-
species (e.g. Clarke, 1973: Valvata sincera on-
tariensis Baker). Recently collected specimens
(juveniles-adults) from one of Hubricht's insolita
localities (2 November, 1985; Meramec Spring,
8 km southeast of St. James, Phelps County,
Missouri) were examined and found to exhibit
considerable variability with regards to the dis-
tinguishing characters for insolita. In no case
was there any evidence of an uncoiled body
whorl. Palmer (1985 and references within)
demonstrated that shell variation in gastropods
can be strongly influenced by environmental
conditions and/or intraspecific genetic plasitici-
ty and does not necessarily reflect divergence
(i.e. speciation). The distribution of insolita
(from Hubricht, 1940) is not geographically
distinct from that of aldrichi s.s. Considering
the above, itisolifa does not appear to warrant
subspecific status in the modern sense (see
Mayr, 1966).
Morton (1967) and many others have dis-
cussed problems related to constructing mollus-
can classifications from single-based systems
(e.g. shell morphology). As noted above, varia-
tion in shell characters does not always imply
speciation (Palmer, 1985). Conversely, lack of
shell morphological variance is not always in-
dicative of conspecificity or close phylogenetic
relationships, but may mask divergent or con-
vergent evolution (Davis, 1979; Dillon and
Davis, 1980; Vail, 1980; Thompson, 1984).
Hubricht (1940) was unable to readily differen-
tiate shells of his third subspecies, Amnicola
aldrichi antroecetes. from slender examples of
aldrichi s.s. Both the previously discussed
"subspecies" are epigean forms with pigmented
bodies and functional eyes; however, antroecetes
is an unpigmented, blind, obligate troglobite.
Hubricht (1940) failed to be consistant in his
methodology for distingTiishing the subspecies
of A. aldrichi: insolita i)y shell characters vs.
antroecetes by anatomy and operculum. Even
though insolita is considered invalid, this devia-
tion still suggests that different levels of
organization were being examined. Thompson
100(1
At)iMl :-!(), Ut8C.
THE NAUTILUS
it
(1984) indicated that "a hi.u'h degree of
anatiitnical uniformity" exists within groups of
the Hydrobiidae (e.g. Lithoglyi.)hinae). The loss
of pigmentation and eyes represents a rather
radical divergence from the epigean anatomy of
aldrichi s.s. To consider these troglohitic ada]>
tations to be ecophenotypic variation implies an
amazing genetic plasticity and an "use it or lose
it" evolutionary interpretation. Ecophenotypic
variation does not meet modern criteria for sub-
specific status (Mayr, 1966); however, previous
relegation of nntroeretes as a subspecies reflects
the over-reliance on shell characters for con-
structing phylogenies. Amnicola antroecefes
should be considered a distinct species. In-
terestingly, A. iintriieceteii has a rather wide
distribution when compared to other regional
troglobitic gastropods (restricted to single or
connected caves). Other troglobitic taxa (e.g.
Amblyopsidae; Isopoda: Caecidotea) exhibit
similarly wide ranges in the Interior Highlands.
This may be related to the karst geology of the
region. Hubricht (1940) did note some size varia-
tion at different localities liut correlated this to
food availability. However, due to its wide range
he suggested that .4. antn)ecefe>< may represent
a composite group. Further investigation is ob-
viously warranted for the A. aldrichi complex
and, for that matter, the Hydrobiidae through-
out the Interior Highlands.
Acknowledgments
The uniqueness of Somatogyrus roi^ewnteri
was confirmed by Fred G. Thompson, Florida
State Museum, University of Florida. SEM's
were prepared with the assistance of Claudia S.
Bailey and specimens o{ Amnicola aldrichi were
provided by Michael L. Mathis, both Depart-
ment of Zoology, University of Arkansas.
LITERATURE CITED
Baker. F. C. 1928, The fresh-water Mollusca of Wisconsin,
part 1: Gastropoda. BulL Wiitc. Geol. Nat. Hist. Sun:
70:1-507.
Burch. J. B. and J. L. Tottenham. 1980. North American
Ireshvvatcr snails; species Hst. runnes, and illustratinns.
W.ilbrniir, \:S]--l\r,.
Clarke, A. 11. 197M. The freshwatei' molluscs of the Cana<lian
Interior Basin. Mulnaihiyin 13:1-509.
Davis, G. M. 1979. The origin and evolution of the gastropod
family Pomatiopsidae, with emphasis on the Mekong River
Triculinae. Aaid. Nut. Sri. Phil. Monoiji: 20:1-120.
Dillon. R. T. and G. M, Davis, 1980. The Gimwlmxiit of south-
ern Virginia and northwestern North (Carolina: genetic
and shell morphometric relationshijis. Mnlacolitijtti
20:83-98.
Gordon, M. E. 1980, p'reshwater Mollusca of the Elk River,
White River above Beaver Reservoir, and Frog Bayou
drainages of the southwestern Ozarks. Unpublished M,S,
thesis. University of Arkansas, .366 pp.
1981, Recent Mollusca of Arkansas with annota-
tions to systematics and zoogeography, Proc. Ark. Anid.
Sri. 34(1980):.5S-62.
Hinkley, A, A, 1915, New fresh-water shells from the Ozark
.Mountains. Pruc. U.S. Nail. Mm.s, 49:587-589.
Hershler. R, 1985, Systematic revision of the Hydrobiidae
(Gastropoda: Rissoacea) of the Cuarto Cienegas basin,
Goahuila. Mexico, Malacologia 26:31-123,
Hershler, R, and G. M. Davis, 1980, The morphologv' of
Hudrobia Irunrata (Gastropoda: Hydroliiidae): relevance
to systematics of Hi/drohia. Biol. Bull. 158:19.5-219.
Huliricht, L. 1940, The Ozark amnicolas. Tin- Naiililiis
53:118-122,
1971, New Hydrobiidae from Ozark caves, 77/r
Naiitilii.<: 83:93-96,
1979, A new species of Amnicola from an Arkan-
sas cave (Hydrobiidae). The Naalil ua 94:14S
Mayr. E. 1966. Animal species and evolutinn. The Belknap
Press of Harvard University Press, Cambridge. 797 \)]).
Morton, .J, E, 1967, Molluscs. Hutchinson and Company,
Ltd,, London, 244 pp.
Palmer, A, R, 1985, Quantum changes in gastropod shell
morphology need not reflect speciation, Eroliitiou
39:699-705,
Sampson. F, A, 1913, A preliminary list of the Mollusca of
Missouri (exclusive of the Unioniade), Tmn.s, Acad. Sci.
St. Lo)(),s 22:67-108,
Thompson. F, G, 1977, The hydrobiid genus Marstonia.
Bull. Fla. Slate Mus. (Bi(j|, Sci,) 21:113-1.58,
1984, North American freshwater snail genera
of the hydrobiid subfamily Lithoglyphinae. Malacologia
25:109-141,
Vail. V, A, 1980. The species problem in Campeloiiia (Gas-
tropoda: Viviparidae), Bull. Amer. Malacol. Union
1979:67,
Walker, B, 1915, Apical characters in Somatogyrus. with
descriptions of three new species. The Nautilus 29:37-41,
49-.53,
Wheeler, H, E, 1918. The Mollusca of Clark County. Arkan-
sas. The Nautilus 31:109-125.
78 THE NAUTILUS
April 30, 1986
Vol. 100(2)
FAVARTIA BREVICULA (SOWERBY, 1834) AND TWO NEW SPECIES
OF FAVARTIA FROM THE WESTERN PACIFIC
(GASTROPODA: MURICIDAE)
Anthony D'Attilio and Barbara W. Myers
Department of Marine Invertebrates
San Diego Natural History Museum
San Diego, CA 92112
ABSTRACT
Murex breviculus Sowerby, 18SJt, is reexamined and a lectotype is selected from
the syntypic lot. Murex tetragonus Broderip, 1833, is discussed and it is our con-
clusioyi the name is a nomen dubium. Two 7iew species of Favartia Jousseaume,
1880, are described, one from the Solomons one from the Philippines.
The identity of Murex breviculv^s Sowerby,
1834, has never been in doubt and the figure in
the Conrhological Illustrations (Sowerby, 1834,
pi. 63, fig. 37) clearly defines the species. The
illustration agrees with the brief but adequate
description published later in the Proceedings of
the Zoological Society of London (1841:146-i47J.
The syntypic lot consisting of three specimens
was borrowed from the British Museum. A
lectotype was selected and the two remaining
specimens are considered paralectotypes. For
purposes of clarity all three specimens from the
type lot are illustrated herein through the
courtesy of the Trustees of the British Museum
(Natural History).
The identity of Murex tetragonus Broderip,
1833, on the other hand has never been estab-
lished. Broderip's description in the Proceedings
of the Zoological Society of London for 1832,
was based on a single "very much waterworn"
specimen. Broderip did not figure this species,
but Sowerby (1834) figured M. tetragonus in the
Conchological Illustrations (pi. 61, fig. 25 and pi.
63, fig. 36). We were informed by Ms. Kathie
Way of the Molluscan Section, British Museum,
that they were unable to locate any type
material of M. tetragonus Broderip.
Institutional abbreviations used in this paper
are: ANSP = Academy of Natural Sciences
Philadelphia. BM(NH) = British Museum
Natural History. SDNHM = San Diego Natural
History Museum.
Muricidae Rafinescjue, 1815
Muricopsinae Radwin and D'Attilio, 1971
Favartia Jousseaume, 1880
Type Species: Funirtin brcricula (Sowerby, 1834)
by original designation
Favartia brevicula (Sowerby, 1834)
Murex brevirulus Sowerby, 1834: Conch. 111. PI. 63. fig. 37
Figs. 1-8, 13
The syntypic lot oi Favartia brevicula (Sower-
by, 1834) borrowed from the British Museum
(NH) consisted of three beach eroded specimens
reg. #1974088.
The lectotype, measuring 26 mm x 20 mm,
was selected because it had the least amount of
erosion. Shell is broadly biconic, the number of
whorls indeterminate because of the erosion of
the spire. Whorls convex, aperture subcircular,
smooth within, inner lip erect, outer lip crenu-
late, reflecting external cords, anal sulcus not
apparent, canal narrowly open, broad, moderate
in length, terminally sharply recurved: three
older canal terminations on fasciole; four broad
varices crossing shoulder and abutting whorl
above; narrow intervarical areas appear smooth
on lectotype; leading edge of varices reaching
midway in the intervarical area; varices deeply
cut and depressed on both leading and receding
side; where varix crosses the shoulder it is
bladelike and strongly recurved; the leading side
of the varix with longitudinal lamellae un-
dulating between the spiral cords; five thick
spiral cords on body whorl, obsolete in narrow
intervarical areas, the first three about equal
size, the two anterior ones small and grouped as
a pair. Two minor cords on the canal separated
by a gap from the body cords at the base of the
l)ody whorl. Color of types is dull-white.
Vol. 100(2)
April 30, 1986
THE NAUTILUS 79
p'KiS. l-(i. Fiirnrtiii hriTiruUi (Siiwerliy. 1X34).
1, Dorsal and 2, apertural views of lectotype
BM(NH) #lii74088 (26.0 x 20.0 mm.); 3 and 4,
paralectotype BM(NH) #1974088 (23.75 x 17.0
mm.); 5 and 6. paralectotype BM(NH) #1974088
(26.75 X 20.0 mm.).
FIGS. 7 and 8. Farartlit hirrirulii (Sowerby. 1834)
SDNHM 76669 small specimen from Bohol Straits, Philip-
pine Islands. 7, protoconch; 8, general shell morphology
(11.0 mm X 7.4 mm.).
Type Locality -Unknown. The species if
found throughout the western and south Pacific
to east Africa.
Dimensions -
BM(NH) #1974088 ■
BM(NH) #1974088
BM(NH) #1974088 ■
Length Width
26.0 mm X 20.0 mm
23.75 mnix 17.0 mm
26.75 mm X 20. 0 mm
Lectotype
Paralectotype
Paralectotype
DisciLSsion - So-werhy (1879) in the Thesaurus
Conchyliorwn appeared to change the descrip-
tion of F. hrevicula. Instead of having four
varices as described in the original description,
he stated there were five varices for F.
hrevicula. Although the three syntypes for F.
brevicula have only four varices and in most of
the specimens examined there were only four
varices, among the material at our disposal, we
found nine specimens with five varices from dif-
19 :- ■, 20
FIGS. 19 and 20. F. Mmgonn Broderip. 1833, taken from
Sowerby (1834). 19, from pi. 61, fig. 25; 20, from pi. 63,
fig. 36.
80 THE NAUTILUS
April 30, 1986
Vol. 100(2)
ferent localities and ranging in size from 11.5
mm to 23.0 mm. The number of varices appears
to be a variable character.
Favartia tetragona (Broderip, 1833)
Murex tetragonus Broderip. 1833: Proc. Ciimm. Sci.
Corresp. Zool. Soc. London. 174.
Figs. 19, 20
The single specimen available to Broderip was
in poor condition and the only one he ever saw.
It was never figured by Broderip and the
description is not definitive. The original
description is as follows:
Mliiie\ TETiiAUONl'l,. MuT . tcstd pt/Tamtdali, albidA, ouadri-
Jaruim tancosn, tranivrrtim caslatu, suLcaucellatu ; apcrturit
violacca, protmncnte ; iabii Umbo unduloio-crmutato ; canali
Lrevi, recurvd ; long. \i, lot. J poll.
Hab.y
Mu£ Sowerbv
'J'his sppcinicn. the onlv one 1 ever saw, is ver\' much watet-
worn, but llie leadinfr cliarnclers of lliu tuecie.', ore uiiiniurtL
W. J. I..
According to Broderip the habitat was un-
known. The specimen was deposited in Museum
Sowerby and its whereabouts today is unknown.
The illustrations by Sowerby in 1834 (PI. 63, fig.
36 and PL 61, fig. 25) do not show a waterworn
shell as described by Broderip, but do show a
very pyramidal-shaped shell, with a broad base
and flaring lip. Figs. 19 and 20 are copied from
Sowerby (1834).
Lacking typological material the morphology
of this taxon must rely entirely on Broderip's
description and the figure by Sowerby. Reeve
(1845: PI. 26, fig. 18) figured the broad coarse
shell of Murex breviculuH Sowerby placing M.
hreviculus in the synonymy of M. tetragonus. the
earlier name, stating he could not discover "any
s{)ecific differences between Murex tetragonuH
and hreviculuH". Sowerby who did the illustra-
tions for the Conchologia Iconica did not dispute
the synonymy. However, in 1879, in the
Thesaurus Conchyliorum. Sowerby included
both binomens {Murex tetragonuti sp. 187, fig.
228 and M. hreviculus sp. 188, fig. 229), and in
comparing the two species stated at that time
that M. hreviculus was a shorter and thicker
shell than M. tetragonus and had five varices.
This differed from M. tetragonus which was de-
scribed as having four varices. In 1879 Sowerby
also stated for M. tetragonus that the latticed
varices follow from whorl to whorl so conflu-
ently as to form four oblique walls up the spire
and he stated for M. breviculu^s "ad spiram inter-
ruptis".
The identification of M. tetragonus has never
been established. As stated above Reeve (1845)
synonymized M. hreviculus with M. tetragonua.
the earlier name. Tryon (1880: pi. 36, fig. 424,
425) agreed with Reeve, figuring both the broad
heavy shell of Af. hreviculus and what looks like
a copy of Sowerby's figure of M. tetragonus,
both under the name of M. tetragonus.
In recent works the following authors figured
what they believed to beF. tetrngona as follows:
Smith, M. (1939: pi. 6, fig. 2) figured F.
hrevicula.
Cernohorsky (1967: pi. 15, fig. 20) figured an
undetermined species.
Fair (1976: pi. 20, fig. 295) figured an undeter-
mined species.
Radwin and D'Attilio (1976) mistakenly de-
scribed F. tetrngona as having three varices and
figured it on pi. 14, fig. 3. This is the new species
described here as F. trivaricosa and shown also
in text fig. 96 of Radwin and D'Attilio.
Inasmuch as there is apparently no type ex-
tant for F. tetragona, the identity of the species
has not been established in 150 years. We have
not been able to associate Sowerby's figure with
any species of Favartia known to us and we
believe this species is of dubious merit, therefore
we are placing it among the doubtful names. It
is interesting to note that no authors, to date,
have mentioned Broderip's description of the
aperture being prominently violet.
Favartia robertsoni new species
Figs. 9-12, 14, 15. 16
Shell medium size, broadly fusoid, spire mod-
erately high, anterior truncate, approximately
five whorls, early whorls eroded; protoconch not
determined; weakly shouldered, somewhat tabu-
late; shoulder area between the varices de-
pressed and concave, especially on receding side
of the varix; suture impressed; body whorl
broader than high; aperture subovate; peris-
tome erect; outer lip undulate, reflecting exter-
nal transverse cords; canal broad, very narrowly
open, short, terminally tube-like, bent backward
nearly at right angle; siphonal fasciole retaining
two older canal terminations.
Varices thick, four per whorl; intervarical
Vol. 100(2)
April 30, 1986
THE NAUTILUS 81
■1
1
1
^^^^^^^MiS^
w'PV
^^1
W^^
i^
\%
HP^^Hk-^^
^"^^
-^i^k
Ei^^ V^^jj|i
mm
■
Kf^*^
mm
H
^^^1^^^^^
■
1 11 1
FIGS. 9-12. 9, 10, Fiivartin rohi-ii^oiu n. sp. holotype SDNHM 86944 (26.0 >
26.5 mm.). 11 and 12, paratype Din the Donald Pisor collection (26.6x27.2 mm.;
areas with moderately raised cords; varices ex-
tending over shoulder obliquely to left and ter-
minating at suture.
Spiral sculpture as follows: one broad cord at
the shoulder prolonged prominently into a blunt
spine, the margin nearly closed on the leading
side; a similar broad cord below extending
beyond the varix, but not prolonged into a spine,
up to the penultimate varix. On the mature
apertural varix these two cords do not project
beyond the remaining sculpture of the varix.
Four secondary cords on the body whorl dimin-
ishing in size anteriorly; varix deeply excavated
between the cords on receding side; cords on
body whorl more or less weakly raised; three
minor cords on shoulder obsolete except near
apertural varix. Leading side of varices re-
curved and with scabrous lamellae producing a
surface with squarish pits; weak scabrous
lamellae on surface of spiral cords between
varices.
Color: Creamy white entirely except for the
holotype with is a dead collected shell lightly
stained with rust.
Type Locality -Ma.\si\t2. Island, Solomon
Islands.
Dimensions- LenKth width
Holotype SDNHM 8B944
.Ataa, Malaita Island, Solomon Is. 2t;.l) 21) 5 mm
Paratype A, SDNHM 86942
Marau Sound, Guadalcanal, Solomon Is. 17,0 1,5,',)
I'aratype B, ANSP 289.'JBK
Malaita Island, Solomon Islands 2(1, .5 20,2
82 THE NAUTILUS
April 30, 1986
Vol. 100(2)
KKjS. lIMti. 13, Outline drawinn' <if Furnrtiii hrcriruhi
(Sowerby, 1884) SDNHM 78704 (19.6 x 15.2 mm.). FIGS.
14-16, Fnvartia nibcrtsoni D'Attilio and Myers. 14,
paratype B ANSP 289568 (20.5 x 20.2 mm.); 15, paratype C
ANSI' 289568 showing micro.sculpture of receding side of
varix; 16, leading side of varix.
f'aratyiif C, ANSI' '289568
Malaita Island. Solomon Islands 14.4 14 1
Paratype D. Donald Pisor collection.
Malaita Island. Solomon Lslands 26.6 27.2
Paratype E, Glass and Foster collection
Marau Sound. t'lUadalcanal, .Solomon is. 24.5 1.75
Etymology -This species is named for Dr.
Robert Robertson, Curator and holder of the
Pilsbry Chair of Malacology', Academy of
Natural Sciences Philadelphia, whose mala-
cological insight the senior author has long ad-
mired.
D i.sTM.s.s?o« - The varices appear the same ex-
cept when fully mature; it is only at maturity
that the final varix shows its character as in the
above description. Comparison is made with its
nearest congener, F. brevicula (Sowerby, 1834),
which has a thicker, coarser shell with a broader
more obese body whorl and larger aperture. F.
brevicula lacks the extended long heavy spine on
the varices previous to the mature apertural
varix. It also has no noticeable keel on the
shoulder and has five equal cords on the body
whorl in contrast to the two major cords and
four secondary cords of F. robertson i.
F. robertsoni new species was figured in
Radwin and D'Attilio (1976) pi. 23, fig. 1 1 and pi.
24, fig. 2 as F. brevicula (Sowerliy, 1834).
Favartia trivaricosa new species
Figs. 17, 18
Shell small fusoid, spire high, anterior trun-
cate, approximately seven whorls: protoconch
eroded, not determined; suture impressed.
Aperture ovate, peristome erect anteriorly, but
appressed posteriorly on the inner side; outer lip
crenulate reflecting external transverse cords,
canal short very narrowly open, terminally tube-
like and bent backward nearly at right angle,
siphonal fascicle retaining one older canal ter-
mination.
Varices moderately thick, three per whorl on
the final and penultimate whorl, four on the
earlier whorls; varices extending over shoulder
and terminating at suture. Intervarical areas
with axial sculpture in the form of low, flat,
thickened lamellae. Sjiiral sculpture as follows:
one cord above the shoulder and four broad
cords on the Ixxly whorl. Leading side of the
varices recurved and with scal)rous lamellae,
deeply excavated between the cords on the
receding side. A combination of the axial
Vol. 100(2)
April 30, 1986
THE NAUTILUS 83
FICS. 17 and 18. Famrtid trivancoxa n. sp. hulotype SDNHM 86943 (15.0 x
VI. 4 mm.).
lamellae crossed by these spiral cords results in
square pits in the intervarical areas. When worn
only the pits are visible.
Color: Dull-white varices with very pale-tan
intervarical areas; aperture pale lavender.
Type Locality-Boho\ Straits, Philippine
Islands.
Drmensions-
Leiiifth
Width
nini.
mm.
Hcilotype SDNHM 8ill»43
Bohol Straits. P. 1. (ex Foster and Class)
\bM X
0.4
Paratype A, SDNHM 8205)4
Celm Island, P. 1.
13..5 X
9.4
Paratype B, SDNHM 737(12
Bohol Straits. P. I.
13.0 X
H..'')
Paratype C. SDNHM 76(i(i8
Mactan Island, P. I.
12.0 X
fi.B
Paratype D. SDNHM 8227e
Mactan Island. P. I-
14.3 X
9.7
Paratype E.
Glass and Foster eollection. P. I.
13.0 X
8.7
Other Material Era mined -One specimen in
the June King collection from Bohol Straits, P.
I. (11.0 X 6.0 mm.); one specimen in the Rose
D'Attilio collection from Wading Island, Fiji
Islands (18.3 x 11.4 mm).
Discussion - Comparison is made with the fol-
lowing species ol Favartia:
F. alveata (Kiener, 1842) from the West Indies
which has five to seven varices instead of three
as does F. trivaricosa, and spiral cords orna-
mented with scales appressed to their surface.
F. brevicula (Sowerby, 1834) which is a broad
heavy larger shell with four or five broad sculp-
tured varices and smooth intervarical areas.
F. cyclostoma (Sowerby, 1841) which is a large
shell with five varices.
F. minatauros Radwin and D'Attilio, 1976
from Mauritius which has an obtuse spire and a
swollen body whorl.
F. mundit (Reeve, 1849) from Japan which has
four to five varices.
F. trivaricosa new species was mistakenly
figured in Radwin and D'Attilio (1976) pi. 14,
fig. 3 and text fig. 96 as F. tetragona (Broderip,
1833).
Etymology -Th\s new species is named for the
three varices on the body whorl which distin-
guish it from several of its congeners. Latin tri
(three) plus varicosa (varices).
Acknowledgments
We wish to thank the following for the loan of
typological and comparison material: Academy
of Natural Sciences Philadelphia; American
Museum of Natural History, British Museum
(Natural History); Rose D'Attilio; June King and
Donald Pisor of San Diego, California; and
Charles Glass and Robert Foster of Santa
Barbara, California. We also thank David K.
Mulliner for the photography used in this paper.
William K. Emerson and Walter E. Sage, III
kindly reviewed the paper.
LITERATURE CITED
Broderip, W. ,1. 183.3. Characters of new species of Mollusca
and Conchifera collected liy H. Cuming. Proc. Cunim. Sci.
Corrpitp. Ziiiil. S'ic. Lmuldii for 1832. pp. 173-179.
84 THE NAUTILUS
April 30, 1986
Vol. 100(2)
Cernohorsky. W. (). 1967. The Muricidae of Fiji. Vi'ligcr
10(2):1 11-132, pis. 14-15.
Fair, R. 1976. The Murcx Book: an illustrated catalogue (if
Recent Muricidae (Muricinae. Muricopsinae. Ocenelirinae)
138 pp., 23 pis.
.lousseaume, F. 1880. Division methodiqiie de la famille des
Purpurides. Le Naturaliste 42:335-336.
Kiener, L. C. 1842-43. Species general et icdnoyniphie ilea
ciKjiiiUen ririniti's 7, Rocher (MH/v':r), pp. 1-130, pis. 1-47.
Fiadwin. G. and A. U'Attilio. 1976. Murex shells of the
World, an illustrated guide to the Muricidae. Stanford
University Press. 284 pp.. 32 pis., 192 text figs.
Rafinesque, C. S. 1815. Analyse de la. nature ou tableau dii
univers et des corps organises. Barravecchia, Palermo.
Reeve, L. 1849. Conch. Iconica vol. Ill, Murex, errata ad
fiiirni. Index.
Smith, M. 1939. An illustrated cataloij of the recent species
of the rock shell. Muricidae, Thaisidae and Coralliophilidae.
Lantana, Florida. 34 pp., 21 pis.
Sowerby, G. B. (second of name). 1834. Conch. Illust. Murex.
London, pis. .58-67.
1841. Descriptions of some new species of
Murex. principally from the collection of H. Cuming, ESQ.
Pj'oc ZooI. Soc. London, pp. 137-147.
1879. Thesaurus Conrhyliorum. London, vol. 4,
55 pp., 24 pis.
Tryon, G. W., .Ir. 1880. Manual ofConcholoipi Philadelphia,
vol. 2, 289 pp., 70 pis.
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CONTENTS^'
THE
NAUTILUS
Volume 100, number 3 - July 30, 1986
ISSN 0028-1344
M. G. Harasewych and Richard E. Petit
Notes on the Morphology of Admete viridula (Gastropoda: Cancellariidae) .
.85
Ian Stupakoff
Observations on the Feeding Behavior of the Gastropod Pleuroploca princeps
(Fasciolariidae) in the Galapagos Islands
.92
William K. Emerson
A New Species of Morum from the Andaman Sea (Gastropoda: Volutacea).
.96
Antonio J. Ferreira
A New Deep- Water Species of Lepidoplewrus (Polyplacophora) from the Venezuela Basin 98
William K. Emerson and Walter E. Sage III
A New Species of Lyria (Gastropoda: Volutidae) from the Arabian Sea 101
David Nicol and Douglas S. Jones
Litharca lithodomus and Adaptive Radiation in Arcacean Pelecypods.
.105
W. Labato Paraense
The Radula of Acrorhis petricola (Pulmonata: Planorbidae) .
,109
Harald A. Rehder
Natica (Glyphepthema) tedbayeri, a replacement name .
112
Book Reviews 91, 104, 113, 114
NEW MANUSCRIPTS
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Spring, MD 20901-0430. The list of Consulting Editors will remain largely the
same, and Dr. Abbott will continue as an Associate Editor beginning with
volume 101.
A HISTORY OF
SHELL COLLECTING
S. Peter Dance
In addition to being an historical
classic, this book answers a
thousand trivia! questions:
A NEW AND ESSENTIAL
SOURCE BOOK
An intriguing history of shell collecting and
conchology, from pre-historic times up to the
twentieth century. A scholarly and exciting
description of early expeditions, infamous shell
collectors of the past, and the story of the strug-
gles and triumphs of early conchologists. This
newly illustrated and expanded book, with a
more complete bibliography, with an enlarged
American section, and with an appendix to the
whereabouts of over 600 famous, old shell collec-
tions, is a continuation of Peter Dances' well-
known history of shell collecting.
I'uhlishi-cl in IDKK l.y K J Hrill ,.f Hull.iii.l ami iliMnlmU'il in North Ami-rita iiy
AMERICAN MALACOLOGISTS
(New Englanii Division)
P.O. Box 1192
Burlington, Mass. 0180;Miy2
280 pp., 32 pis. (1 in color), text figs. Hardbound.
U.S. $39.50.
Who invented the words concholofjy and malacology, and
when?
How did Capt. James Cooke's ship collect the first known
Sunburst .Shell in New Zealand?
What French conchologist pawned the family silverware
in order to buy a rare Spondylus Thorny Oyster?
What happened to the valuable shell collection of the widow
of Capt. Bligh of mutiny fame?
How was Linnaeus duped into naming a common acid-
treated cowrie as a new species?
What beautiful English Duchess with the greatest shell
collection used to entertain King George 111 at breakfast?
And what ancient Roman author gave us the words, Tellina,
I'urjmra and Nerila?
Who has the world's record for collecting the most new
.species of marine and land shells?
Vol. 100(3)
July 30, 1986
THE NAUTILUS 85
NOTES ON THE MORPHOLOGY OF ADMETE VIRIDULA
(GASTROPODA: CANCELLARHDAE)
M. G. Harasewych and Richard E. Petit'
Department of Invertebrate Zoology
National Museum of Natural History
Smithsonian Institution
Washington, DC 20560
ABSTRACT
The anatomy and shell morphology o/ Admete viridula (Fabricius, 1780), a
boreal cancellariid, are described. This species, the type o/ Admete Kroyer, 18^2,
differs from members of the Cancellariinae and Trigonostominae in having a
thinner shell composed of a single aragonitic layer, a reduced kidney and jaw, and
a long, expanded prostate gland, as well as in lacking a radula, separate sperm
ingesting gland and dorsally recurved albumen gland. Based on cladistic analysis
of 20 shell and anatomical characters, we suggest that the family Admetinae is an
early offshoot from primitive cancellariid stock, that the subfamily Trigono-
stominae contains the most primitive cancellariids studied anatomically to date,
and that Cancellariinae comprise a comparatively recent radiation with
specialized chemosensory capabilities.
The composition and taxonomic history of the
superfamily Cancellariacea have been briefly
discussed in previous papers (Harasewych &
Petit, 1982, 1984). The relationship of this group
to other prosobranchs is still uncertain, as is the
phylogenetic arrangement of the nearly 100
nominal supraspecific taxa proposed almost ex-
clusively on the basis of shell characters.
Recent supraspecific taxa have, in general,
been clustered around three morphological
types, represented by the genera Cancellaria.
Trigonostoma and Admete, that have been given
subfamily status by Cossmann (1899). Members
of the Cancellariinae and Trigonostominae in-
habit tropical and temperate waters while
Admetinae is generally limited to polar regions
with some species inhabiting deeper waters of
the temperate zone. The gross anatomy of
Cancellaria reticulata (Linne, 1767), the type of
Cancellariinae, and Olssonella smithii (Dall,
1888) a trigonostomine, have previously been
described (Harasewych and Petit, 1982, 1984).
No general anatomical studies of any adme-
tine are known to us, although brief descriptions
of the animal of Admete viridula (Fabricius,
1780) were given by Moller (1842: 88, as A.
'Research Associate. P.O. Box 30, North Myrtle Beach, SC
29582.
crispa Moller) and Jeffreys (1876: 322). Simple
drawings of the living animal were published by
H. & A. Adams (1853: pi. 29, fig. 5; copied by
Tryon, 1885: pi. 7, fig. 32), Troschel (1865: pi. 4,
fig. 14) and Morse (1921: pi. 7, fig. 43). Troschel
(1865: pi. 4, figs. 16, 17) figured the jaws of A.
viridula and the synonymous A. crispa, refer-
ring to these structures as "hard apparatus" and
suggesting that they may be toxoglossan
radular teeth. The latter figure was copied by
Fischer (1883: 595, fig. 359) and labelled as a
radular tooth. Tryon (1885: pi. 7, fig. 33) copied
Fischer's figure without comment. Thiele (1904:
172) identified Troschel's figures as jaws and
reported the absence of a radula in A. viridula.
The austral species A. magellanica Strebel,
1905, and Waipaoa marwicki Dell, 1956, were
shown to lack radulae, respectively, by Powell
(1951: 167) and Beu and Climo (1974: 327). Not
all admetines are without radulae as evidenced
by the figures of the radula of Nothoadmete
tumida Oliver, 1982, that accompanied the
description of that species. The gross anatomy
and shell morphology of Admete viridula
(Fabricius, 1780), the type species of Admete
Moller, 1842 [as A. crispa Moller, 1842] are here
described and compared to other cancellariid
taxa.
The checkered nomenclatural history of this
86 THE NAUTILUS
July 30, 1986
Vol. 100 (3)
species is detailed by Bouchet & Waren (1985:
257), who point out that North American
authors have used the junior synonym Admete
couthouyi (Jay, 1839) for the species, based on
incorrect statements by Dall (1887: 298; 1918:
318, 328) contending that the type of ^4. viridula
was a turrid. Although this was refuted by
Pilsbry (1938), Macpherson (1971: 107), citing
Dall, followed other New World malacologists in
using j4. couthouyi.
Admete viridula is exceedingly variable as at-
tested by the synonymy listed by Bouchet &
Waren (1985: 258), to which additional nomina
will eventually be added. While the Canadian
specimens used for this study are not "typical" of
the species, in conchological characters, they do
fall within the range of variation accepted by
Bouchet & Waren (1985: figs. 683-689) who ex-
amined thousands of North Atlantic specimens.
Materials and Methods
Anatomical data is based on 20" and 19
specimens from the Saguenay River, Quebec
[48°24'48"N, 70°44'-70°48'W] Voucher Material-
National Museum of Natural Sciences, Ottawa
43946.
Shell fragments for ultrastructural studies
were broken from the outer lip with pliers.
Specimens were then immersed in 10% hydro-
chloric acid (HCl) until the shells dissolved. Soft
parts were rinsed in distilled water and returned
to 70% ethanol for dissection. Portions of the
reproductive systems and anterior proboscis
were sectioned at a thickness of 6 ^m, and the
sections stained in hematoxylin and eosin. Dried
shell fragments were powdered in a mortar and
pestle, and the X-ray diffraction pattern deter-
mined on a Philips APD 3600 Automated X-ray
Powder Diffractimeter.
Shell Morphology
External: Shell, reaching 20 mm in length,
thin, ovate with conical spire and rounded
anterior (Fig. 1). Protoconch (Figs. 3, 4) pauci-
spiral, consisting of 1 whorl, with a smooth,
chalky surface incised by fine, spiral lines. Tran-
sition to teleoconch marked by beginning of
axial growth striae and an increase in shell
thickness. Teleoconch with up to 5V2 convex
whorls. Early whorls (Fig. 2) strongly shoul-
dered, becoming more rounded with increase in
shell size. Suture deeply impressed. Spiral
sculpture of 16-21 shallow, rounded cords on
body whorl and 7-10 on the penultimate whorl.
Axial sculpture of 14-24 ribs per whorl, increas-
ing in number but decreasing in prominence as
the shell becomes larger. Aperture elliptical,
deflected from coiling axis by 20-28°. Outer lip
smooth to slightly corrugated. Siphonal canal
short but pronounced in juveniles (Fig. 2), com-
monly indiscernible in large adults (Fig. 1).
Inner lip with 2 weak columellar folds and a
siphonal fold. Color white to ivory, uniform
within and without.
Internal: Fractured shells revealed the inter-
nal surfaces to be smooth and continuous, and to
lack the apertural lirae and periodic increases in
prominence of columellar folds found in other
cancellariids (Harasewych and Petit, 1982,
1984).
Ultrastructure: A thin, brownish, lamellose
periostracum overlies the shell, which appears
to consist of a single layer of crossed-lamellar
crystals (Fig. 5), oriented with lamellar planes
parallel to the outer lip. X-ray diffraction
analysis of powdered shell revealed it to consist
primarily (>95%) of aragonite.
Soft-parts Morphology
External features: The soft-parts comprise 3
to 3V3 whorls, of which the digestive gland (Fig.
7, dg) occupies about 2V4 whorls, the kidney
(Fig. 7, k) less than Vs whorl and the mantle cavi-
ty just over V2 whorl. Preserved animals were
orange tan in color, lacked any discernible
markings and were retracted at most 'A whorl
into the aperture. The foot is broad and ovate,
lacking an operculum. Tentacles (Fig. 7, t) are
long, tubular and symmetrical. The mantle edge
is smooth, the siphon (Fig. 7, s) short but
distinct.
Mantle rarity: The mantle cavity is shorter
and broader than in other cancellariids dis-
sected, with pallial organs situated as in other
higher prosobranchs. The osphradium (Fig. 7,
os) is broad anteriorly (L/W = 3), tapers
posteriorly, and consists of about 35 leaflets per
side. Adjacent is the ctendium (Fig. 7, ct), twice
as long and slightly narrower than the
osphradium, composed of about 70 triangular
leaflets. This organ and the voluminous, trans-
versely pleated hypobranchial gland (Fig. 7, hg)
Vol. 100(3)
July 30, 1986
THE NAUTILUS 87
FIGS. 1-6. Features of the shells and jaw of Adniete viridula (Fabricius). 1, Apertural and right side views of specimen
collected in the Saguenay River, Quebec. [48°24'48"N, 70°44'-70°48'W] sta. 62 30 (NMNS 43946) 3.0 x . 2, Scanning elec-
tron micrograph of juvenile specimen dredged in 673 m, off Martha's Vmeyard, Massachussetts, U.S. Fish. Comm. sta.
994-97. (USNM 43232) 20.0 x . 3, Protoconch of specimen in figure 2, lateral view, scale bar = 200 ^jm. 4, Protoconch of
specimen in figure 2, axial view, scale bar = 200 /jm. 5, Fracture surface. Plane of fracture parallel to outer lip, scale bar
= 100 fjm. 6, Lateral view of jaw. scale bar = 50 jjm.
88 THE NAUTILUS
Vol. 100(3)
vd pap
rmc
FIGS. 7-10. Anatomical features of Admete oiridula. 7, Female specimen removed from shell, partially un-
coiled and mantle cavity opened mid-dorsally to display contents. 8, Dissection of anterior portion of proboscis,
opened mid-dorsally. 9, Diagrammatic representation of the alimentary system. 10, Male reproductive system.
a, anus; ag, albumen gland; asg, accessory salivary gland; be, bursa copulatrix; bg, buccal ganglia; bm, buccal
mass; eg, capsule gland; ct, ctenidium; dg, digestive gland; hg, hypobranchial gland; int, intestine; j, jaw; k,
kidney; m, mouth; me, mid-esophagus; ng, nephridial gland; nr, nerve ring; opm, opening to mantle cavity; os,
osphradium; ot, oral tube; pap, papilla; pc, pericardium; pen, penis; pr, prostate gland; r, rectum; rmc, rear of
mantle cavity; s, siphon; sg, salivary gland; sto, stomach; sv, seminal vesicle; t, tentacle; tes, testes; vd, vas
deferens; vl, valve of Leiblein.
span the roof of the mantle cavity. The pallial
gonoducts and rectum (Fig. 7, r) are located
along the right side of the mantle cavity, while
its rear is formed by the pericardium (Fig. 7, pc)
and kidney (Fig. 7, k). The kidney is small, being
only twice the size of the pericardium. The
nephridial gland (Fig. 7, ng) occupies nearly half
the kidney along the pericardium.
Alimentary system: The broad, tubular pleu-
rombolic proboscis can be extended nearly the
length of the shell aperture, and is the same
color as the foot. Broad retractor muscles ex-
tend from the columellar muscle, while thinner
strands originate from the body wall. A short
oral tube (Fig. 8, ot) extends from the mouth
(Fig. 8, m) to the cuticularized, tubular portion
of the jaw (Fig. 8, j), which expands posteriorly
to envelope the lateral surfaces of the minute
buccal mass (Fig. 8, bm). The longitudinally
grooved buccal mass lacks a radula and has only
a vestigial subradular membrane. A pair of
short, extremely thin accessory salivary glands
(Fig. 8, asg) lie alongside the buccal mass,
emptying into the posterior portion of the oral
tube through fine ducts. The wider and much
longer salivary glands (Fig. 8, sg) join the buccal
mass laterally, via short ducts, just anterior to
the esophageal opening. A small valve of
Leiblein (Fig. 8, vl) and a pair of buccal ganglia
(Fig. 8, bg) are situated at the rear of the bucal
mass. The narrow mid-esophagus (Figs. 8, 9,
me) runs posteriorly from the valve of Leiblein,
passing through the nerve ring (Fig. 9, nr)
before expanding and becoming sacular. The
esophagus narrows at the rear of the cephalic
sinus and leads to a simple U-shaped stomach
(Fig. 7, 9, sto) that is embedded in the anterior
face of the digestive gland. Longitudinal folds
Vol. 100(3)
July 30, 1986
THE NAUTILUS 89
TABLE 1. Admete rindutn (Fabricius), measurements of
shell characters. Linear measurements in millimeters, (n =
10).
Standard
Character Mean Deviation Range
shell length
16.87
1.91
13.82-19.02
shell width
9.90
1.13
8.18-10.97
aperture length
10.21
1.42
8.13-11.58
aperture length
0.604
0.023
0.567-0.641
shell length
#whorls, teleoconch
4.78
0.35
4.33-5.33
spire angle
.5.5.2°
2.9°
45.5°-.58.0°
line the stomach and pass into the intestine (Fig.
9, int), which runs through the kidney and along
the right wall of the mantle cavity, expanding
slightly to form the rectum (Figs. 7, 9, r).
Neither an anal gland nor identifiable gut con-
tents were detected in any of the specimens ex-
amined.
Female reproductive system: As the only
female specimen available to us was poorly pre-
served, only the pallial portion of the oviduct is
described. The oviduct passes through the
kidney and expands to form a broad, laterally
compressed albumen gland (Fig. 7, ag), which
expands further to form the long, blunt, capsule
gland (Fig. 7, eg). A small, ovate, bursa copula-
trix (Fig. 7, be) is situated below the anterior
margin of the capsule gland. An ingesting gland
was not found. Egg capsules oi Admete viridula
are figured by Bouchet and Waren (1985: fig.
687).
Male reproductive system: The testes (Fig. 10,
te) consist of a yellowish mass of ascinous
tubules embedded in the right side of the diges-
tive gland and extend nearly a full whorl from
its anterior edge. These tubules converge to
form a testicular duct that immediately forms a
serpentine seminal vesicle (Fig. 10, sv). The duct
straightens at the anterior limit of the digestive
gland, passes through the kidney and enters the
mantle cavity ventral to the rectum. It greatly
expands to form the prostate gland (Fig. 10, pr),
which extends along the posterior third of the
mantle cavity and communicates with it by a
long ventral slit (Fig. 10, opm). From the
anterior portion of the prostate gland, a tubular
vas deferens (Fig. 10, vd) leads to the base of the
penis (Fig. 10, pen), which is ovate in cross-
section, extends approximately % the length of
the mantle cavity and has a terminal papilla
(Fig. 10, pap).
Nervous system: Admete viridula has a typical
cancellariid nervous system (Bouvier, 1887:
Harasewych and Petit, 1982, 1984), with the
cerebral, pedal and pleural and subesophageal
ganglia fused into a nerve ring, and the buccal
ganglia (Fig. 8, bg) at the rear of the buccal
mass.
Discussion
Cladistic analysis of the 20 shell and
anatomical characters listed in Table 2 produced
the cladogram in Figure 11. Despite the lack of
agreement on the relationships of supraspecific
taxa, nearly all classifications proposed to date
separate the Admetinae from the remaining
Cancellariidae (H. and A. Adams, 1853:
Troschel, 1865; Fischer, 1883; Tryon, 1885;
Cossmann, 1899; Thiele, 1929; Wenz, 1943), and
this arrangement is supported by the present
study.
Of the characters used to distinguish the
Admetinae from other cancellariids, most con-
TABLE 2. Shell and anatomical characters used to distin-
guish between Admete viridula, Cancellaria reticulata and
Olssonella smithii. Primitive states denoted by (0), derived
states by (1).
1) Shell: (0) thick: (1) thin.
2) Internal varices: (0) pronounced; (1) reduced or absent.
3) Shell ultrastructure of: (0) 2 orthogonal layers; (1) 1
layer.
4) Protoconch of: (0) 2 whorls; (1) 1 whorl.
5) Tentacles: (0) symmetrical, unmodified; (1) asymmetri-
cal, left tentacle modified.
6) Osphradium with approximately: (0) 35 leaflets/side; (1)
70 leaflets/side.
7) Ctenidium with: (0) < 125 leaflets; (1) > 200 leaflets.
8) Distance between osphradium and ctenidium: (0) nor-
mal; (1) large relative to either organ.
9) Kidney occupying; (0) > 'A whorl; (1) < Vs whorl.
10) Proboscis: (0) tubular; (1) ventrally flattened, papillose.
11) Jaws with: (0) short posterior lobes; (1) long posterior
lobes.
12) Buccal mass: (0) small; (1) large, filling retracted pro-
boscis.
13) Radula: (0) present; (1) absent.
14) Outer cusps of radular teeth: (0) simple, smooth; (1)
with secondary dentition.
15) Accessory salivary gland: (0) shorter than; (1) longer
than; salivary gland.
16) Mid-esophagus posterior to nerve ring: (0| sacular; (1)
convoluted tube.
17) Anal gland: (0) present; (1) absent.
18) Sperm ingesting gland: (0) present; (1) absent.
19) Albumen gland: (0) dorsally recurved; (1) laterally com-
pressed.
20) Prostate gland: (0) long, expanded; (1) short, con-
voluted.
90 THE NAUTILUS
July 30, 1986
Vol. 100 (3)
3
•o
>
CO
w
3
o
o
CJ
E
FIG. 11. Cladogram of phylogenetic relationships of cancel-
lariid taxa. Single slashes across tree branches represent
transformations of the corresponding character from the
primitive (0) to the derived (1) state. Double slashes indicate
transformations that occur more than once.
spicuous are their thin shells lacking pro-
nounced surface sculpture and apertural lirae.
This is likely a consequence of their polar
habitat, as Graus (1974) has shown that de-
creased calcification in high latitudes is due to
reduced availability of calcium carbonate in
colder waters. Admetines also lack such anti-
predatory features as internal varices that are
found in tropical and temperate cancellariids.
The predominance of aragonite in the shell is
plesiomorphic, as calcite is more easily formed
(Wilbur, 1964) and more stable (Lowenstam,
1954) at low temperatures.
In terms of anatomical organization, Admete
viridula differs from ancestral cancellariid mor-
phology, most nearly approximated by Olsso-
nella snulhii of the taxa studied to date, in hav-
ing a shallower mantle cavity, a reduced kidney,
and in lacking color pattern. At least some of
these may also be adaptations to cold water.
Cancellariines and Trigonostomines have uni-
serial "tricusped" radular teeth with elaborate
secondary dentition on the outer cusps and a
comparatively simple ventrally recurved central
cusp (Harasewych and Petit, 1982, 1984; Petit
and Harasewych, 1986). The radula of Notho-
admete tumida, the only known radulate
admetine, has barbed central cusps and simple
bulbous outer cusps (Oliver, 1982: figs. 3, 5).
Presence of central cusp barbs in Cancellaria
atopodonta Petit and Harasewych (1986: figs.
15, 16) suggests that this feature is primitive
and occurred in the ancestor of all Recent
cancellariids. The jaws of admetines lack the
long posterior lobes found in cancellariines and
trigonostomines. Although the diet of cancel-
lariids remains unknown, we have suggested
that they are piercing suctorial feeders based on
the functional morphology of their alimentary
systems (Harasewych and Petit, 1982, 1984;
Petit and Harasewych, 1986). The loss of radula
and reduction in the size of the buccal mass in
most admetines suggests that they feed suc-
torially, but on a different group of prey
organisms than other cancellariids.
The lack of an anal gland in Admete viridula
and Cancellaria reticulata is likely a com-
paratively recent convergence, as this organ has
been reported in Cancellaria cancellata
(Graham, 1966).
Additional differences between admetines and
other cancellariids are found in the reproductive
systems. The prostate gland ofAdynete viridula
is long and greatly expanded, while in Olssonella
smithii and Cancellaria reticulata it is short and
convoluted. Admete viridula also lacks the
separate sperm ingesting gland and dorsally
recurved albumen gland found in cancellariines
and trigonostomines.
The phylogenetic arrangement in Figure 1 1 is
supported by the fossil record, as several
"admetines" have been reported from the Upper
Cretaceous, and Waipaoa. known to be
aradulate in the Recent fauna, dates back to the
Oligocene. Cancellaria, sensu stricto, first ap-
pears in the Miocene and is characterized by
modifications to the left cephalic tentacle, pro-
boscis, osphradium and ctendium, organs in-
volved in tactile and distance chemoreception.
Acknowledgments
We thank Jane B. Topping, Invertebrate
Zoology Division, National Museum of Natural
Sciences, Ottawa, for making available the
preserved specimens used in this study. Some of
this work was done at the Smithsonian Marine
Station at Link Port, Florida, and we thank Dr.
Vol. 100(3)
July 30, 1986
THE NAUTILUS 91
Mary Rice for making these facilities available.
This is contribution number 158 of the Smith-
sonian Marine Station at Link Port. Critical
review of the manuscript by Dr. R. S. Houbrick,
National Museum of Natural History, Smith-
sonian Institution, is gratefully acknowledged.
LITERATURE CITED
Adams, H. and A. Adams. 1853-58. The Getiera of Recent
MoUusca. 3 vols. London.
Beu, A. G. and F. M. Climo. 1974. Mollusca from a recent
coral community in Palliser Bay, Cook Strait. N. Z. Joum.
Marine and Freshwater Research 8(2):307-332.
Bouchet, P. and A. Waren. 1985. Revision of the Northeast
Atlantic Bathyal and Abyssal Neogastropoda excluding
Turridae (Mollusca, Gastropoda). Boll. Malacologico.
Suppl. 1:121-296.
Bouvier, E. L. 1887. Systeme nerveux. morphologie
generale et classification des Gasteropodes prosobranches.
Ann. Sci. nat. Zool. 3:1-510.
Cossmann, M. 1899. Caneellariidae. Essais de Paleocon-
chologie Ccmiparee 3:1-41, pis. 1-2.
Dall, W. H. 1887. Supplementary notes on some species of
mollusks of the Bering Sea and vicinity. Proc. U.S. Nat.
Miis. 9:297-309, pis. 3-4.
1888. [in] Agassiz, A. Three Cruises of the United
States Coast and Geodetic Survey Steamer Blake, 2(8):
62-75, figs. 282-312.
1918. Notes on the nomenclature of the mollusks
of the family Turridae. Proc. U.S. Nat. Mus. 54:313-333.
Dell, R. K. 1956. The Archibenthal Mollusca of New Zealand.
Dominion Mus. Bull. 18:1-235, pis. 1-25, A, B.
Fabricius, 0. 1780. Fauna Groenlandica. Hafnia et Lipsiae.
452 p.
Fischer, P. 1880-1887. Manuel de conchyhologie et de
paleontologie conchyliologique ou histoire naturelle des
moUusques vivants etfossil.es. Paris, F. Savy. 1369 p.
Graham, A. 1966. The fore-gut of some marginellid and can-
cellariid prosobranchs. Stud. trop. Oceanogr. Miami
4:134-151.
Graus, R. R. 1974. Latitudinal trends in the shell character-
istics of marine gastropods. Lethaia 7:303-314.
Harasewych, M. G. and R. E. Petit. 1982. Notes on the mor-
phology of Cancellaria reticulata (Gastropoda: Caneellari-
idae). The Nautilus 96(3):104-113.
1984. Notes on the morphology of Olssonella
smithii (Gastropoda: Caneellariidae). The Nautilus
98(l):37-44.
.Jay, J. C. 1839. A catalogue of the shells . . . contained in the
collection of John C. Jay. M.D. Ed. 3, New York. 125 p.,
10 pis.
Jeffreys, J. G. 1876. New and peculiar mollusca of the Euli-
midae and other families of gastropoda, as well as the
pteropoda, procured in the 'Valerous' expedition. Ann.
Mag. nat. Hist. 4(19):317-339.
Linne, C. von. 1767. Systema naturae per regna tria
naturae. Editio duodecimo reformata. Vol. 1 (2):
533-1327. Stockholm.
Lowenstam, H. A. 1954. Factors affecting the aragonite:
calcite ratios in carbonate secreting marine organisms. J.
Geol. 62:284-322.
Macpherson, E. 1971. The Marine Molluscs of Arctic
Canada. Nat. Mus. Canada, Publ. in Biol. Oceanography,
No. 3:1-149.
Moller, H. P. C. 1842. Index Molluscorum Groenlandiae.
Nat. Tidsskr. 4:76-97.
Morse, E. S. 1921. Observations on living gastropods of New
England. Peabody Museum, Salem. 29 pp., 9 pis.
Oliver, P. G. 1982. A new species of Cancellariid gastropod
from Antarctica with a description of the radula. Br.
Antarct. Surv. Bull. 57:15-20.
Petit, R. E. and M. G. Harasewych. 1986. New Philippine
Caneellariidae (Gastropoda: Cancellariacea), with notes on
the fine structure and function of the nematoglossan
radula. The Veliger 28(4):436-443.
Pilsbry, H. A. 1938. On the history and status oi Lora Gistel.
The Nautilus 51(4):11.5-118.
Powell, A. W. B. 1951. Antarctic and Subantarctic Mollusca:
Pelecypoda and Gastropoda. Discovery Repts. 26:47-196,
pis. 5-10.
Strebel, H. 1905. Beitrage zur Kenntnis der Mollusken
Fauna der Magalhaen-Provinz. Zool. Jb., Abt. Syst., Jena
22:575-666, pis. 21-24.
Thiele, J. 1903 [1904]. Die beschalten Gastropoden der
deutschen Tiefsee-Expedition 1898-1899. B. Anatomisch-
systematische Untersuchungen einiger Gastropoden.
Deutsche Tiefsee-Exped.. Bd. VII:149-179, Taf. 1-9.
1929-35. Handbuch der system.ati.'ichen Weich-
tierkunde. Jena, Gustave Fischer. 1154 p.
Troschel, F. H. 1856-1893. Das Gebiss der Schnecken. zur
Begriindung einer natilrlichen Classification. 2. Berlin.
Tryon, G. W. 1885. Family Caneellariidae. Manual ofCon-
chology 7:65-98, pis. 1-7.
Wenz, W. 1938-1943. Handbuch der Paldozoologie (0. H.
Schindewolf, ed.), Berlin, Band 6, Teil 1 (pt. 2) 1639 p.
Wilbur, K. M. 1964. Shell formation and regeneration [in]
Physiology of Mollusca, vol. 1, Wilbur, K. M. and C. M.
Yonge eds. Academic Press, New York.
BOOK REVIEW
Washington Public Shore Guide: Marine Waters
by James W. Scott and Melly A. Reuling.
1986. 348 pp., numerous photos, maps and
habitat sketches. Cloth, $25.00; paperback,
$14.95.
If you are planning on studying or visiting the
shorelines of the State of Washington, this is a
great bargain with many useful facts about the
2,400-mile saltwater shoreline of 14 counties. It
largely ignores mollusks, a fact which offers a
challenge to conchologists.-7?. T. Abbott.
92 THE NAUTILUS
July 30, 1986
Vol. 100(3)
OBSERVATIONS ON THE FEEDING BEHAVIOR OF THE GASTROPOD
PLEUROPLOCA PRINCEPS (FASCIOLARIIDAE) IN
THE GALAPAGOS ISLANDS
Ian Stupakoff
Department of Invertebrates
American Museum of Natural History
Central Park West at 79th Street
New York, NY 10024
ABSTRACT
The feeding behavior of the gastropod. Pleuroploca princeps, (Fasciolariidae) is
reported. Eight species of gastropods were found to be preyed upon by P. princeps;
two species of crabs were eaten as carrion. No signs of cannibalism were noticed,
but intraspecific competition was observed.
While working at the marine laboratory of the
Charles Darwin Research Station, Isla Santa
Cruz, Galapagos, Ecuador, I had the opportuni-
ty to collect the gastropod, Pleuroploca princeps
(Sowerby, 1825), (Keen, 1971, p. 611, fig. 1324),
and to study its feeding habits.
The only literature citation on the feeding
habits of P. princeps is by Sorensen (1943, p. 4),
who observed P. princeps feeding on Phyllono-
tus bicolor (now Hexaplex erythrostomus (Swain-
son)) in Bahia San Carlos, Gulf of California.
Other observations on feeding habits are
reported for P. gigantea (Kiener) in the western
Atlantic by Menzel and Nichy (1958, p. 144),
Paine (1963 a, pp. 66, 67; 1963 b, pp. 402, 403),
and Cornellisson (1985, p. 125), and on P.
trapezium (Linnaeus) and P. filamentosa
(Roding) in the Indo-Pacific by Risbec (1932, pp.
374, 375), Maes (1967, p. 51), and Reyes (1981,
p. 4). The major prey items in the diet of
members of the family Fasciolariidae are gas-
tropods, bivalves, sedentary polychaetes, cirri-
pedes and carrion (Taylor, Morris and Taylor,
1980, p. 377, table 1).
Pleuroploca princeps is a characteristic faunal
constituent of the Panamanian province and is
one of the largest gastropods in the Colon
Archipelago (Wellington, 1975, p. 59), attaining
250 mm. in length. This species is widely distri-
buted in the Galapagos Islands. Several
specimens were collected or observed around
the islands of Santa Fe, Santa Cruz, Espahola,
Floreana, Bartolome, Cousins Rock and San
Cristobal. Living specimens were noted in the
subtidal zone and to depths of 21 meters (per-
sonal observation). They were found on lava
rocks or on sandy bottoms but occur more fre-
quently in areas where the lava boulders meet
the sandy bottom.
The specimens of P. princeps used in this
study were collected on lava boulders and sand
at Isla Santa Fe (July, 1984) and Isla Santa Cruz
(Oct. and Nov. 1984). The animals were kept in
aquaria at the marine laboratory.
Feeding Behavior
Since P. princeps is a typical neogastropod, it
feeds mainly on other gastropods (Table 1). Dur-
ing these observations no bivalves were offered
as food. In aquaria, P. princeps were observed
to feed on dead crabs such as Grapsus grapsus
(Linnaeus) and Petrolisthes edwardsii
(Saussure), (see Table 1 and Fig. 2). A specimen
of P. princeps tried several times to attack a
Nerita .^cabricosta (Lamarck) but could not
reach the soft body of the prey with its proboscis
because of the protection of the heavily calcified
operculum of the nerite.
When P. princeps was at rest, the body and
half of the shell was buried in the sandy substra-
tum (personal observation). It was at this
resting time that five specimens of Thais
melones (Duclos) were introduced into the
aquarium as food. By using what are thought to
be chemoreceptors (fide Kohn, 1961), the
predator detected the presence of the prey and
began its search.
The eyes of P. princeps are poorly developed
Vol. 100(3)
July 30, 1986 THE NAUTILUS 93
TABLE 1. Species eaten by Plcurophca princeps in aquarium.
Phylum
Class
Faml ly
Species
MoIIusca
Gastropoda
Cymati idae
Cymatium partheopeum
Thaididae
Thais melones
Purpura columellaris
Purpura pansa
Muricidae
Muricanthus princeps
Tonnldae
Ma lea r ingens
(pers. obs. J. de Roy)
Cypraeidae
Cypraea cervinetta
Conidae
Conus brunneus
Arthropoda
Crustacea
Grapsidae
Grapsus grapsus
Porcellanidae
Petrolisthes edwardsii
and probably cannot visually detect prey. Conse-
quently, this predator must feel its way to the
prey with its massive foot (Fig. A). On contact,
P. princeps wraps the prey in its foot and begins
a series of usually two or three muscular con-
tractions as observed in 20 cases. Raising its
shell slowly and then lowering it very quickly
against its prey (Figs. B and C), the predator
succeeds in making the prey withdraw inside its
shell. When the prey has withdrawn, the shell is
maneuvered until the aperture is positioned up-
ward and close to the predator's proboscis. At
the same time, the predator's muscular foot
closes the prey's siphonal canal which may last
from a few minutes up to two days depending on
the size, shape and strength of the prey (arrow
in Fig. E). Figure 1 shows how P. princeps
envelopes a Cymatium. partheyiopeum (von
Salis) by the same method described above.
When this series of movements is terminated, P.
princeps prys up the prey's operculum with its
proboscis, eventually penetrating the prey's
body and devouring the soft parts (Fig. E). The
whole animal is consumed and the muscular
tissue attached to the operculum is rasped clean
by radular action. Similar feeding habits were
described for Fasciolaria hunteria (Perry),
(Wells, 1958, p. 155) and for Pleuroploca
gigantea (Paine, 1963 a, p. 67).
Competition and Cannibalism
In one of the aquaria, two adult specimens of
P. princeps were deprived of food for a period of
two weeks. During this time no signs of attack
or cannibalism were noticed. No references to
cannibalism by Pleuroploca have been located in
the literature. In contrast, Fasciolaria tulipa
(Linnaeus) (Snyder & Snyder, 1971, p. 257) and
F. hunteria (Wells, 1958, p. 155) will cannibalize
even when other sources of food are available.
Nevertheless, after this period of starvation one
specimen of T. melones was offered as food to
these two specimens. At this moment, competi-
tion was observed between the two P. princeps.
The specimen (approx. 100 mm.) that had
enveloped the prey was then attacked by the
other larger and heavier specimen (approx. 125
mm.) which "unwrapped" the prey and removed
it from its first predator in a period of two
minutes. The smaller predator tried to recover
its prey four times without success.
Acknowledgments
I thank the following people for their
comments on the manuscript: Dr. William K.
Emerson and Mr. Walter E. Sage, III, of the
American Museum of Natural History, Dr. Jan
Pechenick of Tufts University, and Dr. Ruth D.
Turner of Harvard's Museum of Comparative
Zoology, and to Dr. R. Tucker Abbott for editing
this document. I am very grateful to Dr.
Gunther Reck, Director of the Charles Darwin
Research Station, for the wonderful opportunity
to work on the Galapagos Islands. Support in
94 THE NAUTILUS
July 30, 1986
Vol. 100 (3)
FIG. 1, Adult Pleuroploca prinreps (.shell approx. 12r) mm.) ciivflciping a live Cynuitium parthenopeum and closing the
prey's siphonal canal with its muscular foot (see arrow); 2, Adult Pleuroploca princeps feeding on a dead Porcelain crab.
Petrolitkes edwardsii (natural size).
Vol. 100(3)
July 30, 1986
THE NAUTILUS 95
part was received by the Undergraduate-
Graduate Research Program of the American
Museum of Natural History supported by the
Greenwall Foundation.
LITERATURE CITED
Cornellisson, H. 1985. Florida Shelling-Perseverance pays
off! Texas Conchologist 21(4):124-126.
Keen, A. M. 1971. Sea Shells of Tropical West America.
(Second Ed.), Stanford University Press, Stanford, CA.,
xiv + 1064 pp.
Kohn, A. J. 1961. Chemoreception in Gastropod Molluscs.
A7yu;rican Zoologist l(2):291-308.
Maes, V. 0. 1967. Radulae of Two Species of Pleuroploca
(Fasciolariidae) From The Indo-Pacific. The Nautilus
81(2):48-54.
Menzel, R. W. & F. E. Nichy. 1958. Studies of The Distribu-
tion And Feeding Habits of Some Oyster Predators in Alli-
gator Harbor, Florida. Bull. Mar. Sci. Gulf and Caribbean
8(2):125-145.
Paine, R. T. 1963 a. Trophic Relationships of 8 Sympatric
Predatory Gastropods. Ecology 44(l):63-73.
1963 b. Feeding Rate of a Predaceous Gastro-
pod, Ple^iroploca gigantea. Ecology 44(2):402-403.
Reyes, C. W. 1981. The Fascination of Live Shells. Carfel
(Manila) 3(5):4, 10.
Risbec, J. 1932. Note Sur Les Moeurs de Ricinula chaidea
Duel, et de Fasciolaria filamentosa Lmk. Bull. Sac. Zool.
Ft. 57:374-375.
Snyder, N. F. R, & H. A. Snyder. (1971). Pheromone-Medi-
ated Behaviour of Fasfio/aj-ia tulipa. Anim. Behav. 19(2):
257-268.
Sorensen, A. (1943). Traveling and Collecting in Mexico. The
Nautilus 57(l):l-5.
Taylor, J. D., Morris, N. .J, and C. N. Taylor. 1980. Food
Specialization and the Evolution of Predatory Proso-
branch Gastropods. Palaeontology 23(2):375-409.
Wellington, G. M. 1975. Medios Ambientes Marinos Y
Costeros de Galapagos. Ms. on file in library of the Charles
Darwin Research Station. Isla Santa Cruz, Galapagos,
Ecuador.
Wells, H. W. 1958. Predation of Pelecypods and Gastropods
by Fasciolarta huntena (Perry). Bull. Mar. Sci. Gulf and
Caribbean 8(2): 152- 166.
FIG. 3 A-E, Sequence of capturing movements of
Pleuroploca princeps.
96 THE NAUTILUS
July 30, 1986
Vol. 100(3)
A NEW SPECIES OF MORUM FROM THE ANDAMAN SEA
(GASTROPODA: VOLUTACEA)
William K. Emerson
Department of Invertebrates
American Museum of Natural History
New York, NY 10024
ABSTRACT
Morum (Oniscidia) ninomiyai, new species, is described from off Thailand in the
Andaman Sea and is compared with closely related congeners.
In 1981, the late Carl C. Withrow of Florida
submitted to me for identification a specimen of
an apparently new species of Morum from the
Andaman Sea, off southern Thailand. This
unique specimen was subsequently illustrated by
Sally Diana Kaicher (1983) in her "Card
Catalogue of World-Wide Shells", as an ap-
parently undescribed Morum. The Andaman
Sea specimen was again transmitted to me for
study in 1983 by Taizo Ninomiya of Tokyo, who
had obtained Mr. Withrow's collection of
Morum. Mr. Ninomiya kindly permitted me to
retain the specimen with the expectation that
additional material might be forthcoming from
his contacts in Bangkok. Fortunately, a second
specimen resulted from the inquiries of Mr.
Ninomiya, for whom I take great pleasure in
naming this interesting discovery.
The new species is a member of an Indo-
Pacific group within the subgenus Oniscidia
Morch, 1852, composed of the following taxa:
cancellatum (Sowerby, 1824; type species);
grande (A. Adams, 1855); uchiyamai Kuroda
and Habe, in Habe, \^&\\ joelgreenei Emerson,
1981; and watanabei Kosuge, 1981.
The genus Morum (sensu lato) has long been
classified with the mesogastropods in the
Cassidae (Thiele, 1929; Boss, 1982; Emerson,
1985). Anatomical studies of Morum, however,
indicate that this genus is referable to the
neogastropod family Harpidae (Hughes, 1986,
and personal communications). Dr. Hughes has
in preparation a manuscript in which he rectifies
the present taxonomic misplacement of the
genus. Recent observations on New and Old
World species of Morum (sensu stricto and
Oniscidia), moreover, confirm that these
gastropods also autotomize the posterior por-
tion of the foot (R. Goldberg, P. Williams and W.
Liltved, personal communications), a well-
known behavorial characteristic of the' genus
Harpa (Rehder, 1973).
It should be noted that Harpidae Bronn, 1849
(type genus Harpa (Roding, 1798);
(Gastropoda), is a homonym of Harpidae Hawle
and Corda, 1847 (type genus Harpes Goldfuss,
1839) (Trilobita). Raven (1985) has applied to the
International Commission On Zoological
Nomenclature to emend the spelling of this gas-
tropod family to Harpaidae Bronn, 1849 and to
place the emended taxon on the Official List of
Family-Group Names in Zoology.
Morum (Oniscidia) ninomiyai, new species
Figs. 1-5
Morum sp. Kaicher, 1983, #3730, 3 figs., "off Thailand".
(Illustrations of the paratype of this species.)
Diagnosis: Member of the Morum (0.) cancel-
latum (Sowerby, 1824) -M. (0.) watanabei
Kosuge, 1981, complex. Distinguished by having
the outer lip and the thin parietal shield sculp-
tured by numerous, fine, thread-like ridges (Fig.
5).
Description: Shell medium size for genus, at-
taining 40-1- mm in height, pyriform, attenuated
at base. Spire low, extended; protoconch erect
and papillate, composed of IV2 glossy, smooth
whorls. Postnuclear whorls 5 in number, low
conical, weakly shouldered below the suture,
first and second whorls weakly cancellated, sub-
sequent whorls strongly cancellated, with 14
prominent spinose axial ridges per whorl
crossed by 10 moderately weak spiral cords to
form a blade-like, hooked spine at the juncture
of the spiral and axial ribs; spines most promi-
nent at the shoulder. Intervarical areas with 8 to
Vol. 100(3)
July 30, 1986
THE NAUTILUS 97
FIGS. .\-5.Morum (Oniscidia) ninomiyai, new species. 1 and 2, Holotype, AMNH no. 221241. 3-5, Paratype. T. Ninomiya col-
lection (Fig. 5, coated to show sculptural details; photograph courtesy of S. D. Kaieher). 6-9. Morum (Oniscidia) cancellatum
(Sowerby, 1821); after Emerson, 1985, pi. 1, figs. 15-18. 6 and 7, off Taiwan, AMNH no. 183783. 8 and 9, Lectotype, BM(NH)
no. 197744, "China Seas" (photographs courtesy of A. Beu). All figures except figure 5 approximately x 1.
10 evenly spaced axial lamellae. Aperture nar-
row, elongate, semicrescentic in outline.
Parietal shield moderately large, thin with outer
edge raised and covered by numerous, fine, ir-
regular linear lirations, giving the appearance
of fine threads. Outer lip thickened, crenulated
and weakly toothed, with about 10 primary
teeth forming inconspicuous linear projections
on the inner labial margin, 2 secondary teeth
formed between each pair of primary teeth.
Anal sulcus shallow; siphonal canal short, widely
open, weakly recurved. Operculum not known.
Color: Nucleus shiny, buff; postnuclear whorls
with whitish base color, overlaid with flecks of
reddish brown; 4 widely spaced, interrupted
brownish spiral bands on body whorl (1 band on
shoulder, 2 on either side of midbody area, 1
near the base). Aperture milky white; outer lip
and parietal shield white and surface thinly
glazed (in holotype).
Measurements: Holotype, 41.8 mm in height,
25.7 mm in width; paratype, 40.6 mm in height,
25.8 mm in width.
Type locality: off Phuket Island, Thailand
(8°N, 98.22°E), Andaman Sea, dredged in 50 to
150 meters.
Type specimens: holotype, AMNH 221241
(Figs. 1, 2) from type locality; paratype, T.
Ninomiya Collection, from "off Thailand,
Andaman Sea, ex-Carl Withrow Collection,
April 28, 1980", (Figs. 3-5).
Distribution: Known only from the type locali-
ty and adjacent waters.
Remarks: The new species superficially
resembles specimens oi Mo7iim (0.) cancellatum
(Figs. 6, 7, and 8, 9 (lectotype) and M. (0.)
watanabei Kosuge (see Kosuge, 1981, pi. 33,
figs. 1, 2 holotype; Emerson, 1985, figs. 11-14),
but differs in the number of axial and spiral
ridges, the dentition of the outer lip and the
unique sculpture of the parietal shield (Fig. 5).
98 THE NAUTILUS
July 30, 1986
Vol. 100(3)
Acknowledgments
We are grateful to Taizo Ninomiya for
depositing the holotype of this new taxon in the
type collection of moUusks of the American
Museum of Natural History. Richard L.
Goldberg of Fresh Meadows, New York,
William Liltved of San Francisco, California,
and Peggy Williams of Sarasota, Florida kindly
provided information on living Morum observed
or photographed in the field and laboratory.
Their generous cooperation is much appre-
ciated. Alan G. Beu of the New Zealand Geologi-
cal Survey, and Sally Diana Kaicher of St.
Petersburg, Florida, generously provided the
photographs for figures 8, 9 and 5, respectively.
I am also grateful to Dr. Roger N. Hughes of
the University College of North Wales for his
kindness in keeping me informed of his anatom-
ical studies of Morum.
I thank my AMNH colleagues for their con-
tributions to this study: Walter E. Sage HI for
technical assistance, Stephanie Crooms for
word-processing the manuscript, and Stephen
Butler for the photography, except as noted.
LITERATURE CITED
Adams, Arthur 1855. Descriptions of new genera and
species of gasteropodus |.s-(c"] Mollusca. Pror. Zool. Soc.
London for 1853, 21(259): 182-186 (May 16, 1855).
Boss, K. J. 1982. Mollusca, in S. P. Parker, ed., Synopsis
and Classification of Living Organisms, 1 McGraw-Hill
Book Co., New York, pp. 945-1166, illus.
Emerson, W. K. 1981. Two new Indo-Pacific species of
Morum (Gastropoda: Tonnacea). The Nautilus 95(3):
101-105, 7 figs,
1985. Remarks on some western Pacific species
of Morum (Gastropoda: Tonnacea)., in J. M. Lindsay, ed..
Stratigraphy, palaeontology, malacology papers in honour
of Dr. Nell Ludbrook. Spec. Publ. So. Aust. Dept. Mines
and Energy 5, pp. 51-56, 2 pis.
Hughes, R. N. 1986. Anatomy of the foregut of Morum
Roding, 1798 (Gastropoda: Tonnacea) and the taxonomic
misplacement of the genus. The Veliger 29(1), in press.
Kaicher, S. D. 1983. Card Catalogue of World-Wide Shells,
Pack #36, Cassidae & Oocorythidae, card #3730.
Kosuge, Sadao 1981. Descriptions of two new species of the
genus Morum with remarks on the Recent species from
Philippines. Bull. Inst. Malac. Tokyo 1(7):101-104, pi. 33.
Kuroda, Tokubei and Tadashige Habe, in T. Habe. 1961.
Colored Illustrations of the Shells of Japan, 2, Hoikusha,
Osaka, Appendix, p. 1-41.
Morch, 0. A. L. 1852. Catalogus conchyliorum . . . de Yoldi.,
Regis Daniae. Copenhagen. Fac. 1. 170 p.
Raven, J. G. M. 1985. Homonymy in the families Harpidae
Hawle & Corda, 1847 (Trilobita) and Harpidae Bronn,
1849 (Mollusca, Gastropoda). Z.N.(S.) 2331. Bull. Zool.
Nom. 42(l):79-80.
Rehder, H. A, 1973. The family Harpidae of the world. Indo-
Pacific Mollusca 3(16):207-274, pis. 183-247.
Sowerby, G. B. I. 1824. The Genera, of Recent and Fossil
Shells 1, Oniscia, pi. 233.
Thiele, Johannes. 1929. Handbuch der Systematischen
Weichtierkunde. Jena. Bd 1, teil 1. pp. 1-376, 470 text
figs.
A NEW DEEP-WATER SPECIES OF LEPIDOPLEURUS
(POLYPLACOPHORA) FROM THE VENEZUELA BASIN.
Antonio J. Ferreira^
Research Associate, Department of Invertebrate Zoology
California Academy of Sciences
San Francisco, CA 94118
ABSTRACT
A new species o/Lepidopleurus /rom the depths of the Venezuela Basin, Carib-
bean Sea, is described and compared with L. scrippsianus Ferreira. 1980, from
the Eastern Pacific.
From October to December 1981, the Naval
Ocean Research and Development Activity
(NORDA), NSTL Station, MS, conducted in-
'Published posthumously. Died 1986.
tense physical and biological investigations of
deep-sea sediments in the Venezuela Basin from
aboard USNS Bartlett (cruise 1301-82). Among
the benthic macrofauna were 6 specimens of
chitons: 3 specimens, ca. 13, 11, and 9 mm long
Vol. 100(3)
July 30, 1986
THE NAUTILUS 99
3 4 5
FIGS. 1-5, Lepidopleurus bartletti Ferreira, spec nov.: Holotype (USNM 859000), side
view. 2, view of posterior valve. 3, first and second valve. 4, paratype, posterior valve. 5,
paratype, under view, valves i, iv and viii.
(sta. 40: 15°08'N, 69° 12^, depth 3867 to 4009
m, 28 Oct. 1981); 1 specimen, ca. 15 mm long
(sta. 63: 13°45'N, 67°45'W, depth 5046 m, 8
Nov. 1981); 1 specimen, ca. 10 mm long (sta. 65:
13°45'N, 67°45'W, depth 5046 m, 9 Nov. 1981);
and 1 specimen, 1.3 mm long (sta. 88: 13°30'N,
64°45'W, depth 3516 to 3550 m, 25-26 Nov.
1981). All chitons were found on pieces of wood
brought up in trawls. Study of this material,
generously made available through Michael D.
Richardson and Paula M. Mikkelsen, revealed a
new species here allocated to the genus Lepido-
pleurus Risso, 1826.
Order Neoloricata Berhenhayn, 1955
Family Lepidopleuridae Pilsbry, 1892
Genus Lepidopleurus Risso, 1826
Lepidopleurus bartletti Ferreira, spec. nov.
Fibres 1-6
Diagnosis: Small (up to 15 mm long) white
chitons. Valves somewhat rugose; posterior
edges moderately angled; surface covered with
microgranular cuticle over sculptureless, chalky
tegmentum. End valves remarkably flat; mucro
slightly anterior; lateral areas not prominent,
with some concentric growth rugae continuing
into central areas. Gills posterior. Girdle thick;
upper surface carpeted with small spiculoid
elements with occasional, thin, straight, long
spicules interspersed; undersurface reduced to
fine cuticle devoid of scales or spicules. Radula
median teeth wider in back than in front, with
tricuspid major lateral teeth and rakelike
spatulate teeth.
Type material: Holotype (USNM 859000) and
paratypes (CAS 059845; IRCZM 061:085;
LACM 2123).
Other material: Specimen 1.3 x 0.9 mm, from
sta. 88, tentatively identified as L. bartletti
(CAS 059846) but not given paratypic status in
view of its small size and ill-defined, juvenile
characters.
Type locality: Venezuela Basin, Caribbean
Sea, 13°45'N, 67 "45^, at depth of 5046 m.
(Station 63, roughly 150 mi. N.E. of Bonaire,
Netherlands Antilles).
100 THE NAUTILUS
July 30, 1986
Vol. 100(3)
Description: Holotype (from USNV Bartlett
sta. 63), preserved in alcohol, curled, ca. 15 mm
long, 10 mm wide (figs. 1-3). Valves subcarinate,
moderately beaked, with angled posterior
edges. Shell surface covered with microgranular
cuticle, easily scraped off to show chalky white,
sculptureless tegmentum beneath. Anterior
valve remarkably flat. Lateral areas of inter-
mediate valves not prominent except for
greater valve thickness and concentric growth
rugae often continuing unto sculptureless cen-
tral areas. Posterior valve extremely flat; macro
slightly anterior, poorly defined. Gills posterior,
about 20 plumes per side, extending 40% of
length of foot. Girdle creamy white, thick, with
conspicuous straight, thin, glassy spicules inter-
spersed on background of much smaller, thin-
ner, closely packed spiculoid elements.
Paratypes (from USNV Bartlett sta. 40 and
sta. 63.) very similar to holotype. Paratype from
sta. 40, 13 mm long, disarticulated: Cuticle easi-
ly removable from valves uncovering chalky,
sculptureless tegmental surface beneath (fig. 4).
Articulamentum white with no insertion teeth
or slits (fig. 5). Valve i, 5.2 mm wide, 3.2 mm
long, 1.2 mm high at posterior edge. Valve v, 6.0
mm wide, 2.0 mm long in midline. Valve viii, 5.1
mm wide, 3.7 mm long, 1.0 mm high at anterior
edge, slightly convex in premucro area, slightly
concave in postmucro area. Sutural laminae
short, triangular; sinus very wide; on valve viii,
relative width of sinus (width of sutural sinus/
width of sutural lamina) is 1.8. Girdle dorsal sur-
face densely carpeted with blunt-ended, cigar-
shaped, spiculoid elements up to 100 x 25 nm
(up to 120 X 35 ^im at sutures), often longi-
tudinally striated (fig. 6-A), interspersed
straight, vaguely striated, glassy spicules up to
300 X 28 ^m (fig. 6-B), interspersed; undersur-
face reduced to fine cuticle without scales,
spicules or other elements; girdle bridges emp-
ty. Radula 6 mm long, comprising 55 rows of
mature teeth; median teeth (fig. 6-A) 80 ^im
long, 30 ^m wide at anterior blade, enlarging
posteriorly to 60 ^m; first lateral teeth about 80
^<m long, with socketlike concavity at anterior
end; major lateral teeth with tricuspid head (fig.
6-B) about 70 jum wide, 100 jim long at middle
cusp; spatulate teeth 150 ^m wide with fascicu-
late, rakelike appearance (fig. 6-C); outer mar-
ginal teeth 90 ^m long, 120 ^m wide (width/
length, 0.75).
Distribution: Lepidopleurus bartletti is known
only from the general area of the type locality in
the central lower Caribbean at great depths.
Remarks: In addition to L. bartletti, only two
other living species oi Lepidopleurus are known:
L. cajetanus (Poli, 1791), a common intertidal to
sublitoral European species, and L. scrippsia-
nus Ferreira, 1980, collected at over 2500 m in
FIG. 6. Lepidopleurux bartletti Ferreira, spec, nov.: Paratype (CAS 0.')984.5), radular - (A) median and first lateral teeth;
(B) head of major lateral tooth; (C) head of spatulate tooth; (U) interspersed spicule; (E) background spiculoid elements.
Scale bar 100 nm.
Vol. 100(3)
July 30, 1986
THE NAUTILUS 101
the eastern Pacific, SW of Cabo San Lucas, Baja
California, Mexico. A fossil species, L. rnoro-
zakierisis Itoigawa, Nishimoto and Tomida,
1977, is known from the Miocene Morozaki
group of central Japan.
Lepidopleurus bartletti is quite similar to L.
scrippsiayms from which it differs in 1) more
delicate, less rugose valves, 2) posterior edge of
valves forming much wider angle, 3) lateral
areas much less accentuated, 4) extremely flat
end valves, 5) anterior mucro, and 6) valve
covering cuticle [not seen in specimens of L.
scrippsianus], giving bartelli's valves a
microgranular appearance which contrasts with
the sculptureless. chalky tegmental surface
beneath. Notable features common to L. bart-
letti and L. scrippsianus are 1) girdle elements,
2) girdle undersurface reduced to cuticle
without spicules or scales, and 3) radula with
unusually shaped median teeth and rake-like
spatulate teeth.
The species is named bartletti in honor of the
USNS Bartlett for her central role in this study
of the Venezuela Basin.
Acknowledgments
I express my appreciation to Paula M. Mikkel-
sen, Indian River Coastal Zone Museum, Harbor
Branch Foundation, Inc., Fort Pierce, Florida,
who entrusted these specimens to my care and
study. William G. Lyons of Florida's Depart-
ment of Natural Resources very kindly made
many improvements to the manuscript.
LITERATURE CITED
Bergenhayn, J. R. M. 1955. Die fossilen schwedischen
Loricaten nebst einer vorlaufigen Revision des systems
der ganzen Klasse Loricata. Lunds Univ. Arsskrift.
(Avd.2, N.S.) 51 (8):l-43, 2 pits. [Kungl. Fysiogr. Sallsk.
Hand!. N.F. 66 (8):3-42, 2 tables].
Ferreira, A. .J. 1980. A new species of Lepidopleurus Risso,
1826 (Mollusca: Polyplacophora) in the deep waters of the
eastern Pacific. The VeUger 23(1):55-61, 5 text figs., 1 pi.
Gray, J. E. 1821. A natural arrangement of IVIollusca,
according to their internal structure. London Medic.
Repos. 15:229-239.
Itoigawa, J., H. Nishimoto and S. Tomida. 1977. Lepido-
pleurus rtwrozakiensis, a new fossil Polyplacophora
from the Miocene Morozaki group, central Japan. Bull.
Mizunami FossU Mus. 4:55-59, 2 text figs., pis. 14-15.
Pilsbry. H. A. 1892. Polyplacophora. Manual of Conchology
14:1-64; pits. 1-15.
Poli, I. X. 1791-1827. Testacea utrisque Siciliae eorumque
historia et anatome tabulis aeneis illustrata. Vol. 1 (1791).
Risso, A. 1826. Histoire naturelle des principales produc-
tions de I'Europe Meridionale et particulierement de
celles des environs de Nice et des Alpes maritimes. Vol.
4, 439 pp., 12 pits., 183 figs. Paris & Strasbourg: F.-G.
Levrault. 5 vols.
A NEW SPECIES OF LYRIA (GASTROPODA: VOLUTIDAE)
FROM THE ARABIAN SEA
William K. Emerson and Walter E. Sage III
Department of Invertebrates
American Museum of Natural History
New York, NY 10024
ABSTRACT
Lyria leslieboschae, new species, is described from off Masirah Island,
Sultanate of Oman, Arabian Sea. Known only from a few beach specimens, this
new taxon is distingwished by discrete differences in shell morphology from the
superficially similar species, Lyria lyraeformis (Swainson, 1821), which occurs
off the coast of Kenya, East Africa.
Donald and Eloise Bosch resided for nearly
thirty years in Oman, where she was a teacher
and he was a practicing physician. During this
time, they became knowledgable shell collectors
and eventually co-authored an illustrated guide,
"Seashells of Oman", which was published in
1983. Among specimens they recently submit-
ted to us for study were four examples of a new
102 THE NAUTILUS
July 30, 1986
Vol. 100(3)
FIGS. 1, 3-5. Hulutype of Lyria kslieboschae new species, AMNH no. 221B5.',. 3-5, dorsal, apertural and oblique views, x 1. 1,
detail of early whorls, x 2.
Vol. 100(3)
July 30, 1986
THE NAUTILUS 103
FIGS. 2, 6-8, Lyria lyraeformis (Swainson. 1821)
oblique views, x 1. 2, detail of early whorls, x2.
trawled off the coast of Kenya, AMNH 21358.3. 6-8, dorsal, apertural, and
species of Lyria found for the first time in
January, 1985, at Masirah Island. We are ex-
tremely pleased to name this exquisite volute in
honor of their daughter-in-law, Mrs. Leslie
Bosch, who actively participated, together with
her husband, David, on ten annual collecting ex-
peditions of the Bosch family to this locality.
Lyria leslieboschae new species
Figs. 1, 3-.5
Diagnosis: In outline and general appearance
the shell resembles Lyria lyraeformis (Swain-
son, 1821, pi. 54, 2 figs.; Weaver and duPont,
1970, pi. 5 A, B; Abbott and Dance, 1982, p. 213,
1 fig.; and Okutani, 1983, pi. 31, fig. 8; here illus-
trated, figs. 2, 6-8), but differs in possessing a
blunt, bulbous nucleus, which lacks a calcarella
(cf. figs. 1, 2), an anal canal that is narrow, open
and flares posteriorly to the region just below
the subsutural spiral band (cf. figs. 4, 7), as well
as by axial sculpture that is less strongly
developed on the body whorl, and a distinctive
color pattern that is more diffused.
Description of holotype, figures 1, 3-5: Shell
large for genus, attaining 130 mm in height,
elongate-fusiform, spire high, attenuated.
Nucleus of 2V2 smooth whorls, without a cal-
carella. Teleoconch of 7V2 rounded whorls, in-
104 THE NAUTILUS
July 30, 1986
Vol. 100 (3)
dented at the suture; axial sculpture weakly
developed on body whorl, numbering 21 on
penultimate whorl, more evenly defined on the
early whorls than on the penultimate and body
whorls. Spiral sculpture best expressed on the
wide, spirally indented subsutural bands, each
with 6 spiral lirae acutely raised at the points of
alignment with the axial ribs. Aperture narrow,
gaping anteriorly, with a short wide siphonal
canal, terminating posteriorly in a long, narrow,
open anal canal, near the base of the spiral band
below the suture. Columella with three anterior
plaits; parietal region without plaits. Exterior
surface above the siphonal canal with 7 spiral
ridges.
Base color a cream-tan, overlaid with inter-
rupted bands of reddish brown formed in the
subsutural areas and on the medial and basal
regions of the body whorl. Reddish brown spiral
lines on the axial ribs. Reddish brown irregular
axial lines on the nucleus. Interior of aperture
and columella glossy, colored a tannish cream,
with a bluish tint. The coloration of live-taken
specimens can be expected to be more vividly
expressed than in this well-preserved beach
specimen, which had several large colonies of
bryozoa encrusting the interior of the aperture
at the time of collection.
Nothing is known of the radula or soft parts.
Measurements: Holotype, AMNH no. 221655,
129.3 mm in height, 38.4 mm in width. Para-
types, AMNH no. 221656, Paratype A, 85.5 mm
in height, 31.3 mm in width, Paratype B, 87.9
mm in height, 31.9 mm in width, Paratype C,
91.8 mm in height, 29.4 mm in width. (The
paratypes lack complete spires).
Type locality: About 8 km south of the village
of Haql, on the southeastern coast of Masirah
Island, Oman.
Distribution: Known only from the tj^De
locality.
Remarks: The only known specimens were
washed ashore by the heavy surf on the Indian
Ocean side of the island. On this exposed beach,
Dr. Bosch {in litteris, May 9, 1986) also reported
finding dead specimens of Festilyria festiva
(Lamarck, 1811) and Conus lischkeanus cf.
tropicensis Coomans and Filmer, 1985, species
which are known to occur in moderately deep
offshore waters. The present species apparently
lives at moderate depths and will require
SCUBA diving and/or dredging operations to
collect living specimens.
Acknowledgments
We thank Dr. and Mrs. Bosch for their kind-
ness in calling to our attention this most elegant
addition to the Volutidae and for depositing the
typological specimens in the type collection of
mollusks of the American Museum of Natural
History. We also thank Stephanie Crooms for
word-processing the manuscript and Stephen
Butler for the photography.
LITERATURE CITED
Abbott, R. T. and Dance, S. P. 1982. Compendium Of Sea-
shells. E. P. Dutton, New York, 411 pp., illus. in color.
Bosch, D. and E, 1982. Seashells Of Oman. Longman Group
Ltd., London and New York, 206 pp., illus. in color.
Okutani, T. 1983. World Seashells of Rarity and Beauty.
Kawamura Collection. National Science Museum, Tokyo,
i-iii + 1-12 pp., 48 pis. in color.
Swainson, W. 1821. Zoolugical Illustrations, London, 1,
pi. 54.
Weaver, C. S. and duPont, J. E. 1970. Living Volutes: a
monograph of Recent Volutidae of the world. Delaware
Mus. Nat. Hist. Mong. Ser., No. 1. xv + 374 pp., 79 col.
pis., 44 figs., 13 maps.
BOOK REVIEW
Hong Kong Seashells by John D. Orr. 1985.
Urban Council, Hong Kong. 122 pp., 94 color
photos. Paperback.
The author presents 60 beautiful, close-up
photographs of living specimens of cowries,
olives, cones, Stromhus conchs and helmet
shells, as well as the shells of 84 other common,
shallow water bivalves and gastropods of the
Hong Kong area. Hints on collecting, classifying
and studying mollusks are included. The spec-
tacular photographs of living specimens make
up for the few included species, lack of authors
and dates, and occasional typographical errors.
Cymatium clandestinum on page 102 is really a
worn Cantharus (Pollia) probably undosa
(Linnaeus, 1758). -/2. T. Abbott.
Vol. 100 (3)
July 30, 1986
THE NAUTILUS 105
LITHARCA LITHODOMUS AND ADAPTIVE RADIATION
IN ARCACEAN PELECYPODS
David Nicol
Box 14376
University Station
Gainesville, FL 32604
and
Douglas S. Jones
Florida State Museum
Gainesville, FL 32611
ABSTRACT
Litharca lithodomus is a rock-boring arcid (subfamily Litharcinae Frizzell,
19Jf6) that has a geographic range from Nicaragua, to Peru. It is not known as a
fossil, and this species may be less than one million years old. Litharca
lithodomus is most likely a mechanical rock-borer. The possible ancestral species
is Barbatia (Cucullaearca) reeveana, which is commonly found throughout the
present range of Litharca lithodomus. Barbatia (Cucullaearca) reeveana nestles
in crevices in rocks and its shape is frequently distorted. The change of habit from
nestling to rock-boring is not great, and this change is seen in some other species
in dijferent families of pelecypods.
The earliest arcaceans, which appeared during the Middle Devonian, were
epibyssate. Shallow-burrowing species of arcaceans probably did not occur before
the Triassic, and nestling species probably appeared no later than the Paleocene.
Fresh-water and rock-boring arcaceans seem to be confined to the Recent.
Many large families or superfamilies of sus-
pension-feeding pelecypods exhibit more adap-
tive radiation than all of the Protobranchia,
which are deposit feeders. One of these large
superfamilies, the Arcacea, is diverse and wide-
ly distributed in the seas today, ranging from
the tropics to the cold water of the Antarctic, as
well as to abyssal and hadal regions.
The earliest true arcaceans appear suddenly
in the Middle Devonian (Givetian Stage) about
380 million years ago. Most paleontologists have
said that the Cyrtodontidae represent the
ancestral stock that gave rise to the arcaceans,
based on the similarity of the hinge teeth and
ligament in some members. A few have doubted
that the cyrtodonts were the ancestors of the
arcaceans (Nicol, 1984). Perhaps a more likely
group to have given rise to the arcaceans was
the Ambonychiidae. Some ambonychiids have
ligaments and hinge teeth similar to the
arcaceans and many were byssally attached
whereas the Cyrtodontidae were burrowers ac-
cording to Stanley (1972). Furthermore, while
the Ambonychiidae were common in the Middle
Devonian, the Cyrtodontidae were nearly ex-
tinct by that time. It is also easier to derive the
byssally attached arcacean Parallelodon from a
byssally attached ambonychiid rather than a
burrowing cyrtodontid.
It is generally agreed that the first arcaceans
were byssally attached to the substrate, and
Parallelodon has a rectangular valve outline
that resembles Area, sensu stricto. Some of the
Paleozoic arcaceans were probably endobyssate,
and this life habit occurred in some species of
Parallelodon. However, arcaceans are not com-
mon and diverse throughout the Paleozoic, and
the great adaptive radiation of this superfamily
began in the Jurassic and continued throughout
the Cretaceous (Nicol, 1984).
The first burrowing arcacean may have been
Macrodontella, which occurs in the Triassic (text
fig. 1). These early burrowing arcaceans did not
appear until at least 150,000,000 years after the
first arcaceans appeared. Other burrowing arca-
ceans occur amongst the cucullaeids in the
Jurassic and Cretaceous, and the glycymeridids
and Trigonarca during the Cretaceous. Some of
the Cretaceous limopsids were probably bur-
rowers but some were endobyssate (Oliver,
1981). Epibyssate, endobyssate, and burrowing
arcaceans continue to the Recent with burrow-
ing species probably outnumbering the epibys-
sate and endobyssate forms.
106 THE NAUTILUS
July 30, 1986
GEOLOGIC
AGE
ROCK-BORING FRESHWATER
BYSSATE NESTLING
Vol. 100(3)
FREE-BURROWING
RECENT
PALEOCENE
(65 mya)
TRIASSIC
(230 mya)
LItharca
DEVONIAN
(380 mya)
• Scaphula
Acar
Macrodontella
Parallelodon
I
I
I
Ambonychlidae ?
FIG. 1 . Diagram showing adaptive radiation in the Arcacea.
Some species of Acar are true nestlers, and
this genus appeared in the Paleocene, about
65,000,000 years ago. Scaphula is an arcacean
that has invaded brackish and fresh water dur-
ing the Recent.
The most unusual adaptation of the arcaceans
occurs in Litharca lithodom.ics (Sowerby, 1833),
a rock-borer (plate 1). The genus is monotypic
and is known only from the Recent. Keen (1971)
stated that the range of the species extends
from Nicaragua to Peru, and it appears to be
most common along the coast of Ecuador.
Olsson (1961) claimed that Litharca is so com-
mon in some areas of Ecuador that fishermen
use it for food and bait. Litharca lithodomus is a
relatively large arcid, and Frizzell (1946) had
one specimen that was 91.1 mm in length.
Olsson (1961) stated that the adult shell reaches
a length of nearly 100 mm.
The shell of Litharca is unusually thick for a
rock-borer, and only some species of rock-boring
tridacnids have slightly thicker shells. In other
words, rock-boring pelecypods commonly have
very thin shells as seen in the mytilids, pholads,
petricolids, and myids. A thin shell may have an
advantage in that it can be more easily and fre-
quently moved within the borehole. Further-
more, a thick shell, as in Mercenaria, is not
needed for protection from carnivorous gastro-
pods and crustaceans. Shells of mechanical rock-
boring pelecypods commonly consist of arago-
nite, but the nacreous structure found in
unionids and Pteriidae is absent. Nacreous
shells are friable and would not be suitable for
mechanical rock boring.
One of the most unusual features of Litharca
lithodomus is the greatly elongated anterior end
(Plate 1). The ligament is wholly prosodetic and
lacks a posterior limb (i.e., the ligament lacks
chevrons). This lack of a posterior limb of the
ligament is also seen in the Cretaceous
glycymeridid Postligata (Nicol and Jones, 1984).
Frizzell (1946) stated that the beaks are slightly
opisthogyrate, but Olsson (1961) said that they
are probably prosogyrate. The beaks are most
likely opisthogyrate because of the prosodetic
ligament and the extreme elongation of the
anterior end of the shell. Prosodetic ligaments
and opisthogyrate beaks are quite common in
glycymeridids. A byssus is present in adult
Vol. 100 (3)
July 30, 1986
THE NAUTILUS 107
055l>)0
PLATE 1. A-D. Litharca lithodomus (Sowerby). Manta, Ecuador. A, Exterior, right valve. B, Interior, left valve. C, Ventral
view, both valves showing small byssal gape (shell length 86.5 mm). D, Dorsal view, both valves showing truncated posterior to
the left. A-D, California Academy Sciences #055190. E-F, Barhatia iCucuUaearca) reeveana (Orbigny). Perlas, Panama. E,
Left valve, exterior. F, Left valve, interior (shell length 79.7 mm). E-F. Florida State Museum #23624.
Litharca lithodomus, but the byssal gape is nar-
row and elongate, and the byssus is flexible so
that the animal is able to move downward in its
borehole (Olsson, 1961). As is shown in Frizzell's
figure 5 (1946), the valves are wedge-shaped
with the most convex portion near the posterior
end. The anterior end is narrow. This is an
unusual shape for a rock-borer.
Thomas (1974, 1976) has assumed that the
boring is accomplished by chemical means in
Litharca. but this may not be so. Both Frizzell
(1946) and Olsson (1961) have observed that
Litharca bores into massive sandstones in
Ecuador. Are these sandstones calcareous or
cemented with calcium carbonate? Field and
laboratory observations on these sandstones
would be essential to come to a final conclusion
as to the mode of boring. Just because Litharca
has a weak ligament and a pitted shell exterior
does not necessarily rule out the possibility that
it may bore mechanically. Furthermore, of the
remaining rock-boring species of pelecypods.
only some species of mytilids bore by chemical
means whereas other species of rock-boring
mytilids are mechanical borers (Yonge, 1951).
Perhaps, as Thomas implies (1976), both
mechanical and chemical means of boring may
be employed by L itharca.
The fact that at least one arcid species has
developed a rock-boring habit is apparently not
as incongruous as it would at first seem. The
two most unusual features found in Litharca
lithodomus that are generally not seen in other
rock-boring species are the posterior displace-
ment of the beaks and the hatchet-shaped con-
vexity of the valves with the most convex region
near the posterior end. Most rock-borers are
cylindrical in shape, and the beaks are either
near the center of the valves or near the
anterior end. The byssus is not unique because
rock-boring mytilids and tridacnids have this
organ developed in the mature rock-boring
stage (Yonge, 1951). Compared to some other
rock-boring pelecypods, Litharca is relatively
108 THE NAUTILUS
July 30, 1986
Vol. 100(3)
unspecialized.
Rock-boring pelecypods are most diverse in
the tropical marine regions. They do not occur
in the abyssal and hadal regions of the oceans
nor in fresh water. There are at least eight
families that have been purported to have one or
more rock-boring species and they are: Arcidae,
Mytilidae, Tridacnidae, Petricolidae, Hiatelli-
dae, Myidae, Gastrochaenidae, and Pholadidae.
The Mytilidae and Pholadidae comprise most of
the rock-boring species, but there are probably
no more than 100 living species of rock-boring
pelecypods. Rock-boring species of pelecypods
are of average to large size. The largest rock-
borers are three species of Tridacna, but they
are the smallest-sized species in the family and
none attains a maximum size of more than about
400 mm. Furthermore, the species that bores
the deepest into the rock is Tridacna
(Chametrachea) crocea Lamarck, and it is the
smallest of the three species, attaining a max-
imum size of only 150 mm (Rosewater, 1965). It
also appears that species of pelecypods that
attain a size of less than 20 mm are not rock
borers, and this may be caused by a lack of bor-
ing capabilities in small-sized species.
It was assumed by Olsson (1961) and Thomas
(1978) that the ancestor of Litharca was a
species of Area. An hypothesis ascribed by
Dechaseaux (1969, p. N765) to Douville is as
follows: "The ancestor was a species living
where its earliest representatives are found and
having some of its distinctive characters." If one
uses this logical principle, then a likely ancestor
to Litharca lithodomus could be Barbatia
(Cuculla^arca) reeveana (Orbigny, 1856) (plate
1). According to Keen (1971), this is a common
species found throughout the present range of
Litharca lithodomus. The ribbing and periostra-
cum of Barbatia (Cucullaearca) reeveana resem-
ble Litharca. The size and convexity of the
valves in the two species are similar. There
would have to be a reduction of the byssal gape
because it is much larger in Barbatia (Cucul-
laearca) reeveana than it is in Litharca. The
beaks of Barbatia (Cucullaearca) reeveana are
commonly subcentral (not near the anterior end
as in Area), and it would require not a great
modification to have the beaks thrust toward
the posterior as in Litharca lithodomus. Bar-
batia (CucullcLearca) reeveana has a habit of at-
taching between rocks (Keen, 1971) so that a
shift to a rock boring habit as in Litharca
lithodomus would be a likely change in adapta-
tion. This is also borne out by Yonge's observa-
tion (1958) that some rock-boring species have
evolved from a byssate nestling species.
Whether Litharca lithodomus will be a short-
lived experiment within the Arcidae or will con-
tinue to evolve and produce more rock-boring
arcids is impossible to assess. As Frizzell
pointed out (1946), the lack of a fossil record of
Litharca lithodomus may be caused by the small
number of rock-boring habitats in the fossil
record and the relatively thin shells of this
species inhibiting preservation. However, the
morphologic changes for the origin of Litharca
lithodomus must have been rapid, and it is quite
possible that the appearance of this species was
less than one million years ago.
Frizzell (1946) erected a separate subfamily,
the Litharcinae, for Litharca lithodomus, and
Yokes (1980) has followed Frizzell in this
classification. We agree with Frizzell and Yokes
because taxonomy should show the differences
as well as the likenesses between species, and
Litharca lithodomus is so unique in morphology
and habit that it merits being placed in a
separate subfamily within the Arcidae.
Acknowledgment
We are indebted to Dr. Peter U. Rodda of the
California Academy of Sciences for granting us
a loan of specimens of Litharca lithodomus for
study.
LITERATURE CITED
Dechaseaux, C. 1969. Hippuritoida-Hippuritacea-Origin and
extinction, p. N765. In Treatise on Invertebrate Paleontol-
ogy. (R. C. Moore, ed.). Part N, Vol. 2, Mollusca 6,
Bivalvia. Univ. Kansas Press, Lawrence.
Frizzell, D. L. 1946. A study of two arcid peleeypod species
from western South America. Jour. PaLeo. 20:38-51.
Keen, A. M. 1971. Sea Shelh of Tropical West America. 2nd
ed. Stanford Univ. Press, California. 1064 p.
Nicol. D. 1984. Changes in the hinge teeth of arcaceans from
Devonian to Recent. Tulane Studies Geol. & Paleo.
18:70-72.
Nicol, D., and D. S. Jones. 1984. Review of Postiigata, a
Late Cretaceous peleeypod. Tulane Studies Geol. & Paleo.
18:67-69.
Oliver, P. (!. 1981. The functional morphology and evolution
of Recent Limopsidae (Bivalvia, Arcoida). Malacologia.
21:61-93.
Olsson, A. A. 1961 . MoUusks of the Tropical Eastern Pacific:
Vol. 100(3)
July 30, 1986
THE NAUTILUS 109
Panamic-Pacific Pelecypoda. Paleontological Research
Institution. Ithaca, New York. 574 p.
Rosewater, J. 1965. The family Tridacnidae in the Indo-
Pacific. Indo-Pacific Mollusca l:347-.396.
Stanley, S. M. 1972. Fuctional morphologj' and evolution of
byssally attached bivalve mollusks. Jour. Paleo.
46:165-202.
Thomas, R. D. K. 1976. Constraints of ligamental growth,
form and function on evolution in the Arcidae (Mollusca:
Bivalvia). Paleobiology 2:64-83.
1978. Shell form and the ecological range of
living and extinct Arcoida. Paleobiolog)'. 4:181-194.
Yokes, H. E. 1980. Genera of the Bivalvia: A Systematic and
Bibliographic Catalogue (Revised and Updated). Paleon-
tological Research Institution. Ithaca, New York. 307 p.
Yonge, C. M. 1951. Marine boring organisms. Research
4:162-167.
1958. Observations on Petricola carditoides
(Conrad). Proc. Malaeological Soc. London 33:25-31.
THE RADULA OF ACRORBIS PETRICOLA
(PULMONATA: PLANORBIDAE)
W. Lobato Paraense
Departamento de Malacologia
Institute Oswaldo Cruz
Caixa Postal 926
20000 Rio de Janeiro, RJ-Brasil
ABSTRACT
Observation of the radular teeth of Acrorbis petricola Odhner, 1937, and A.
odhneri Scott. 1960 with the scanning electron microscope showed no difference
between the two nominal species, which also are indistinguishable in shell and
anatomic characteristics. A. odhneri, therefore, is a junior synonym, of A.
petricola. The radular teeth o/ Acrorbis are similar to those o/Gyraulus, but taxo-
nomically important differences in qualitative characters of the genital system
show that the two geyiera are less closely related than suggested by their radular
characteristics.
Acrorbis petricola is an atypical planorbid
snail described by Odhner (1937) from speci-
mens from Nova Teutonia (27°16'S, 52°20'W), a
village in the Brazilian state of Santa Catarina,
sent to the Swedish Ricksmuseum by the
natural history collector, Herr Fritz Plaumann.
Decisive characteristics for the erection of the
new germs Acrorbis were the Helix-\ike shape of
the shell, and especially the squarish radular
teeth with short hooks (see Fig. 1).
Pilsbry (1938) pointed to the relationship be-
tween Acrorbis and Drepanotrema (misprinted
Drepanostoma) by the similarity of the penial
complex and the presence of a flagellum on the
penial sheath, but distinguished the two genera
by the teeth characteristics as shown by Odhner
(1937).
Baker (1945:123) commented on the alleged
differences in the radular teeth: "The radula [of
Acrorbis] appears very different from that of
Drepanotrema because of the apparent absence
of interstitial cusps between the larger cusps.
These might have been present but overlooked
because of the small size of the radula teeth. The
general shape of the mesocone in Odhner's
figure 4 is suggestive of the same cusp in
Drepanotrema, but the ectocone and entocone
are much shorter." . . . "Acrorbis. therefore,
appears to be another one of the peculiar groups
of South American Planorbidae, related to
Drepanotrema, but distinct by both shell and
anatomy."
Examining specimens from Nova Teutonia,
Hubendick (1955) observed that "though not
very detailed, Odhner's description and figure of
the radula in Acrorbis is not incorrect". His
drawings of a central, a lateral and a marginal
teeth, reproduced in Fig. 2, may be compared
no THE NAUTILUS
July 30, 1986
Vol. 100(3)
&&®SFQ
a^'
.''^^v^
^=^:^
^^^^
^Tryv^
lOjjm
FIGS. 1-4. 1, Radular teeth of Acrorbis petricola reproduced from papers by Odhner, 1937; 2, Hubendick,
1955; 3, Scott, 1960, under the name Acrorbis odhneri; 4, Paraense and Deslandes, 1959. (c, central; i, in-
termediate; 1, lateral; m, marginal. Scale bar refers to Fig. 4).
with Odhner's (Fig. 1).
A redescription of A. petricola, based on
specimens collected at my request by Herr
Plaumann at the same breeding-place from
which the sample studied by Odhner had been
taken, was published by Paraense and
Deslandes (1959). The teeth were represented as
shown in Fig. 4. Accessory cusps can be seen on
either side of the main cusps in the central teeth,
and also between the two main cusps in the fifth
figured central tooth. Spaces wider than usual
appear between the bases of the cusps in several
teeth; such spaces, as later realized, were really
occupied by small cusps which could not be
clearly discerned owing to their minuteness
added to light diffraction effect. After discuss-
ing the anatomic affinities between Acrorbis
and Drepanotrema, Paraense and Deslandes
(1959) concluded that the shape of the shell was
the only character that might warrant separa-
tion of the two genera. Stating, however, that a
revision of the genus Drepanotrema would show
so wide interspecific variation in shell configura-
tion that any generic diagnosis based only on the
shell characters of the type species would be
meaningless, they treated A. petricola. as a
member of Drepanotrema. Subsequently,
Paraense (1975) adopted the genus Acrorbis on
account of its Helix-shaped shell not sculptured
with longitudinal rows of minute dots (puncta-
tion), and of its very long spiral radula project-
ing far beyond the buccal mass.
Under the name Acrorbis odhneri, Scott
(1960) described a snail from Argentina anatom-
ically identical with A. petricola, but differing in
shell characteristics: larger size (largest
specimen 4.25 mm in diameter, as against 2 mm
in Odhner's specimens), rapid whorl growth,
proportionally wider aperture, umbilicus par-
tially covered by the basal reflection of the lip,
and absence of spiral lines on the shell surface.
Scott (1960) states that Odhner so precisely
represented half a teeth row that she could
recognize in it the radula of her own specimens
(Fig. 3). (Translated): "There are no interstitial
teeth between the cusps of the laterals, and the
marginals are markedly short showing no
oblique reflection". Considering the lack of a
long oblique reflection in the marginals suffi-
cient to separate Acrorbis from the Planorbidae,
Scott (1960) created the family Acrorbidae to in-
clude A. petricola and A. odhneri.
On 17 May 1973 I collected 23 specimens of yl.
odhneri at its type-locality, Salto Encantado
(27°03'S, 54°50'W), Departamento Libertador
Oeneral San Martin, Province of Misiones,
Argentina. One may easily reach Salto Encan-
tado by Road 14 (Ruta 14) as far as km 212,
Vol. 100(3)
July 30, 1986
THE NAUTILUS 111
where it intersects Ruta 220 (about 14 km east
of Aristobulo del Valle, Departamento
Cainguas), and then northward by the last-
mentioned road for about 3 km.
Salto Encantado is a waterfall which drops
vertically and sprays the adjacent cliff, favoring
a thick growth of moss where the snail is found.
Such peculiar habitat is similar to that of A.
petricola, which lives among moss on rocky
banks of streams kept wet by trickling water
from the surrounding ground and above the
stream level.
The collected specimens were indistinguish-
able, in shell and anatomy, from A. petricola
from Nova Teutonia, as described by Paraense
and Deslandes (1959). The largest shell was 3.2
mm in diameter. As in the specimens from Nova
Teutonia in our collection, the umbilicus was to
a variable extent covered by the basal reflection
of the lip and the shell surface was more or less
perceptibly sculptured with thin spiral lines.
Other differences mentioned by Scott (1960) as
diagnostic of A. petricola (shell size, rate of
whorl increase, proportion of apertural dia-
meter) can be ascribed to intraspecific or inter-
populational variation.
As to the radula, no significant difference was
observed between the two forms, so that only
teeth of a specimen from Salto Encantado are
shown in Figs. 5-10. As observed with the scan-
ning electron microscope, the central tooth
(Figs. 5, 9) has two dagger-like cusps, of which
the left one is longer than the right; there is one
(sometimes two) minor spine-shaped cusp high
on either lateral side of the major cusps, and
another one between the latter. The laterals
(Fig. 6) have three dagger-like major cusps, of
which the mesocone is much longer, and show
one smaller spine-shaped cusp high on the
lateral side of the ectocone and entocone and
FIGS. 5-lU. Scanning electron micrographs of radular teeth of Acrorbis petricola from Salto Encantado, Misiones
province, Argentina. 5, central (arrow), a little slanted to the right; 6, laterals; 7, intermediates; 8, marginals; 9, central, a
little slanted to the right; 10, marginals. Figs. 5-8, x 29,000; 9, x 25,000; 10, x 20,000.
112 THE NAUTILUS
July 30, 1986
Vol. 100(3)
between the major cusps. Small cusps between
and outside the three major cusps are added
from the intermediates (Fig. 3) to the extreme
marginals (Figs. 4, 6), while the ectocone, the
entocone and particularly the mesocone remain
easily distinguishable. Both major and minor
cusps grow smaller toward the edges of the
radular ribbon. The marginals have short wide
reflections high up on the base of attachment.
The extreme marginals usually show 13-14
cusps, including the three main ones.
The radular teeth of Acrorbis are similar to
those of Gyraulus, recently studied by Meier-
Brook (1983) and Burch and Jeong (1984), but
the absence in Acrorbis of taxonomically impor-
tant characters such as a penial stylet and a
separate prostatic duct, and the presence of
flagella on the penial sheath, show that the two
genera are less closely related than suggested
by their radular characteristics.
The observations described above point to the
identity of A. petricola and A. odhneri, lending
no support to the removal of the genus from the
family Planorbidae.
Acknowledgments
The author is grateful to Petrobras-CENPES
(Centro de Pesquisas e Desenvolvimento) for
use of the facilities of its SEM Laboratory, to
Carlos R. Cordeiro and Flavio J. Versiani for
technical assistance, and to Prof. Walter Berto-
lazzo, Universidade Federal do Rio de Janeiro,
who introduced the author to the staff of the
SEM Laboratory.
LITERATURE CITED
Baker, F. C. 1945. The molluscan family Planorbidae. Univ.
Illinois Press, Urbana. xxxvi + 530 p.
Burch, J. B. and K. H. Jeong. 1984. The radular teeth of
selected Planorbidae. Malacol. Rev. 17:67-84.
Hubendick, B. 1955. Phylogeny in the Planorbidae. Trans.
Zool. Soc. London 28:453-542.
Meier-Brook, C. 1983. Taxonomic studies on Gyraulus
(Gastropoda: Planorbidae). Malacologia 24:1-113.
Odhner, N. H. 1937. Acrorbis petricola n. gen. n. sp., eine
merkliche Siisswasserschnecke aus Brasilien. Ark. Zool.
29B:l-8.
Paraense, W. L. 1975. Estado atual da sistematica dos
planorbideos brasileiros. Arq. Mus. Nac. Rio de Janeiro,
55:105-128.
Paraense, W. L. and N. Deslandes. 1959. The Brazilian
species oi Drepanotrema. VII. D. petricola (Odhner, 1937).
Rev. Brasil Biol. 19:319-329.
Pilsbry, H. A. 1938. Acrorbis petricola. Review. The
Nautilus 51:107.
Scott, M. I. H. 1960. Nueva familia de pulmonado basoma-
toforo (Mollusca). Neotropica 6:65-69.
NATICA (GLYPHEPITHEMA) TEDBAYERI, A REPLACEMENT NAME
Harald A. Rehder
National Museum of Natural History
Smithsonian Institution
Washington, DC 20560
In a recent issue of The Nautilus (Rehder,
1986: Nautilus, 100(1):38) I proposed the name
Natica (Glyphepithema) bayeri for Glyphe-
pithema Jloridana Rehder, 1943, not Natica
Jloridana Dall, 1892.
Now Alan R. Kabat at the Museum of Com-
parative Zoology has kindly called my attention
to the fact that the taxon Natica bayeri is pre-
occupied by Natica (Naticina) bayeri Koper-
berg, 1931 (Jaarboek von het Mijnwezen in
Nederlandsch Oost-Indie, 59: 139, pi. 3, fig. 48)
from the Pliocene of Timor, Indonesia.
I propose now to name the species found, from
southeastern Florida to Brasil, Natica
(Glyphepithema) tedbayeri Rehder.
Vol. 100(3)
July 30, 1986
THE NAUTILUS 113
BOOK REVIEWS
Seashells of Western Australia by Fred E. Wells
and Clayton W. Bryce. 1986. Western Austra-
lian Museum, Perth. 207 pp., 74 colored pis.
Paperback. $17.95 Australian (approx. U.S.
$12.50).
This is an excellent, well-illustrated guide to
the more common and readily found species of
marine mollusks of Western Australia. The
western third of Australia is particularly rich in
molluscan species because of the meeting of the
tropical Indo-Pacific province in the north with
the colder temperate waters of South Australia
and Tasmania. Of the approximate 2000 species
from this region, this accurate guide beautifully
illustrates 671 species, including many photo-
graphs of living specimens of opisthobranchs
and cephalopods. Each family is defined and,
when available, useful bibliographic references
are included. Scientific name, author and date,
size, geographical distribution, relative abun-
dance within Western Australia, and an ex-
cellent photograph are given for each of these
common and conspicuous species. A short in-
troduction on protecting mollusks, cleaning and
maintaining a collection of shells, together with
a glossary and index round out this fine little
book.-/?. T. Abbott.
The Littorinid Molluscs of Mangrove Forests in
the Indo-Pacific Region, by David G. Reid. 24
April 1986. 228 pp., 98 figs., 1 color plate.
Publ. no. 978, British Museum (Natural
History). Cloth, $35.00 (Approximately U.S.
$52.00).
This is one of the most complete and com-
petently executed monographs of a well-known
group of common mangrove-dwelling gastro-
pods. The taxonomy of this otherwise perplex-
ing genus, Littoraria. has been well worked out.
Despite the recognition of 27 Indo-Pacific
species and subspecies in a group heretofore
usually treated as three or four good species, the
author has proposed only two Indo-Pacific new
species, one new subspecies and one new sub-
genus, (Paliistorina). His detailed presentation
of anatomical, egg-capsule, radular and distribu-
tional characteristics will probably lead to a
universal acceptance of his views. Very for-
tunately a large number of earlier names solely
based on shell characters were available for
these new biologically recognized species. Ex-
cellent drawings of penes, pallial oviducts,
sperm nurse cells, and distributional maps ac-
company each of the 27 Indo-Pacific taxa.
Worldwide, 37 taxa are recognized in five sub-
genera of the genus Littoraria Griffith and
Pidgeon, 1834. The first 70 pages of this work
have an excellent discussion of morphological
characters, reproduction, habitats and biogeo-
graphy.-/?. T. Abbott.
It's Easy to Say Crepidula! by Jean M. Cate and
Selma Raskin. 1986. 155 pp. Pretty Penny
Press. P.O. Box 3890, Santa Monica, CA
90403. Paperback, $19.95, plus $1.50 postage.
This is a useful phoenetic guide to the pronun-
ciation of the scientific names of about 3,000
common molluscan taxa. The authors usually
give two pronunciations, one evidently used in
American Latin classrooms, the other used cus-
tomarily among most American malacologists.
Readers may take their choice. However, the
customary pronunciation of the -ae ending, used
in species named for a woman, is not given. The
name myrakeeyiae, for instance, is usually pro-
nounced: MY' ruh KEEN' ee, but the authors
give only MY' ruh KEEN' ay and MY' ru KEEN'
eye. They are correct in suggesting that names
for males, ending in -i, may be pronounced
"eye", as in laurenti: law RENT' eye. There is
also an eleven-page glossary of malacological
terms.-/?. T. Abbott.
Seashell Treasures of the Caribbean by Lesley
Sutty. Edited by R. Tucker Abbott. E. P.
Dutton, New York. 1986. 128 pp., 139 color
plates. $19.95. (with autographed, numbered
bookplate $21.95 from American Malacolo-
gists, P.O. Box 1192, Burlington, MA 01803).
The author, an accomplished naturalist, diver
and photographer, has chosen 100 species of
Caribbean mollusks "to illustrate and comment
upon so that the reader may share my enthu-
siasm and joys in discovering the shells of these
beautiful tropical islands." She has attempted to
inspire others to study mollusks by relating her
experiences in seeking these elusive and fascin-
ating animals in the Lesser Antilles. Her lively
and engaging narrative, coupled with her stun-
ning photographs, are certain to provide any
shell lover with many hours of pleasurable
114 THE NAUTILUS
July 30, 1986
Vol. 100 (3)
reading, and should stimulate interest in seek-
ing and observing marine shells.
A preface by the editor and the author's in-
troduction begin this volume, followed by
chapters entitled, "What is a Rare Shell?",
"Strange and Beautiful Shapes", "Treasures of
Sea and Reef, and "Science in Shells." Rare
shells discussed and illustrated include Cypraea
surinamensis, Pterynotus phyllopterus and
Conies granulatus, to name just a few. Unusual
mollusks, such as Umbraculum umbraculum,
Glossodoris clenchi and Xenophora conchylio-
phorci become familiar through the author's
animated writing style. The bulk of the species
are treated in the "Treasures" chapter where we
meet the rediscovery of Hexaplex straussi and
such desirable species as Lyria archeri, Conus
cedonulli and Chlamys multisquamata. An ab-
breviated history of Caribbean malacology,
followed by a brief bibliography, index and
glossary of terms, completes the text.
There is a great deal of merit in this beautiful-
ly illustrated book, and it is important again to
stress that the author has fully achieved her aim
of sharing with others her collecting activities.
This book is not intended to be an identification
guide. Despite meticulous editing, last minute
publisher's errors do creep in, such as the
transposition of the captions for plates 22 and
23, and the indiscriminate use of parentheses
around every author and date. Nonetheless, it is
hoped that this well-produced and lavishly il-
lustrated work will be enjoyed and appreciated
by nature lovers and conchologists, and will
serve to introduce living mollusks to many new
enthusiasts -Walter E. Sage.
North Atlantic Nudibranchs (MoUusca) Seen By
Henning Lemche by Hanne Just and Malcolm
Edmunds. 1985. 170 pp., 69 pis. in color.
Paperback. Supplement 2 of Ophelia, Inter-
national Journal of Marine Biology, Denmark.
500 kroner (approx. U.S. $60.00)
The excellent 69 color plates depicting the late
Dr. Henning Lemche's personal paintings of 76
of the known 217 species of opisthobranchs of
the North Atlantic will prove useful to students
of nudibranchs. The descriptions of the species
and the information on feeding and reproduc-
tion, together with up-dated taxonomic notes by
the author-editors add considerable usefulness
to the book. A geographical checklist of the 217
species by Elizabeth Platts is very helpful.
Most of Lemche's illustrated species are in the
genera Doto, Onchidoris, Flabellina. Eubran-
chus, Cuthona and Aeolidiella. 26 of the 76
species are given no trivial names and await fur-
ther taxonomic consideration. Perhaps someday
this unfinished book will be carried to conclusion
by one or both of the authors. -i?. T. Abbott.
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REGISTER OF AMERICAN MALACOLOGISTS
OCTOBER 31, 1986
THE
NAUTILUS
ISSN 0028-1344
Vol. 100
No. 4
A quarterly
devoted to
malacology and
the interests of
conchologists
UBRAnr
NOV 4 1986
-- ^SlHoie, Mass.
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Museum of Comparative Zoology
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Department of Geology
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Los Angeles County Museum of Natural History
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Museum of Comparative Zoology
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Dr. G. Alan Solem
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Field Museum of Natural History
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Museum of Zoology
The Ohio State University
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Dr. Ruth D. Turner
Department of Mollusks
Museum of Comparative Zoology
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Division of Biology
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THE
NAUTILUS
Volume 100, number 4 - October 31, 1986
ISSN 0028-1344
CONTENTS "
Louise Russert-Kraemer and Elmer G. Berry
"Things Truly Excellent. . .": Henry Van Der Schalie, 1907-1986 116
R. Tucker Abbott
Cauthdt'us multangulus New Subspecies Grandanus from
Northwest Florida (Buccinidae) 120
Jon-Arne Sneli and Oystein Stokland
On the Taxonomical Status of Tritonium viridulum Fabricius, 1780
(Gastropoda: Cancellariidae) 121
Douglas G. Smith
Pisidium henslowanum (Sheppard) in the Connecticut River,
Massachusetts (Bivalvia: Pisidiidae) 124
C. M. Hawkins and R. B. Angus
Preliminary Observations of Predation on Ocean Quahaugs, Arctictt islandica,
by Atlantic Wolffish, Annrhichas lupu^; 126
Jose D. Gomez. Mercedes Vargas and Emile A. Malek
Freshwater Mollusks of the Dominican Republic 130
Paul W. Parmalee and Walter E. Klippel
A Prehistoric Aboriginal Freshwater Mussel Assemblage from
the Duck River in Middle Tennessee 134
David Nicol
The Fate of Pelecypod Families, Subfamilies, and Tribes During
and After the Cretaceous Period 140
Emile A. Malek
Freshwater and Terrestrial Snails of Saint Lucia, West Indies 143
William K. Emerson and Walter E. Sage III
On the Rediscovery of Teniniiiehin minihilin (Clench and Aguayo, 1941),
and Its Relationship to Other Calliotectine Volutes 147
To Joe Rosewater — from R. Tucker Abbott
Reminiscences 152
All future subscriptions and manuscripts should be sent to Tin
Nautilus. P.O. Box 3430, Silver Spring, MD 20901, U.S.A.
116 THE NAUTILUS
October 31, 1986
Vol. 100(4)
"THINGS TRULY EXCELLENT. . .": HENRY VAN DER SCHALIE,
1907-1986
Louise Russert-Kraemer and Elmer G. Berrv
Henry van der Schalie (1907-1986)
Henry van der Schalie, extraordinary scholar,
teacher and friend to so many of us, died Tues-
day afternoon, 15 April, 1986, in his home near
the Raisin River in Manchester, Michigan, with
his beloved wife and colleague, Annette
Rudolphi van der Schalie, at his side. Born in
1907 in Amsterdam, the Netherlands, Professor
van der Schalie completed high school in Pater-
son, New Jersey, and then earned an A.B.
degree from Calvin College in Minnesota in
1929, an M.S. degree from the University of
Michigan in 1931, and a Ph.D. from the Univer-
sity of Michigan in 1934. At the University of
Michigan, he served from 1929 to 1934 as
Museum Assistant, from 1934 to 1944 as Assis-
tant Curator of Mollusks, and as Curator of
Mollusks from 1944 to 1977. He also held an ap-
pointment as Instructor of Zoology at the
University of Michigan from 1934 to 1937, and
served as Exchange Professor at the University
of Puerto Rico from 1940 to 1944. Returning to
the University of Michigan, he became Assistant
Professor of Zoology in 1944, Associate Pro-
fessor in 1950, and Professor of Zoology in 1957,
a position he held until his retirement in 1977.
Highly respected as an outstanding interna-
tional authority on mollusks, Professor van der
Schalie served on numerous committees and as
consultant to government agencies in Egypt,
Sudan and Japan. He served as a consultant to
the World Health Organization, as well. His
work for these organizations centered on the
mollusk hosts of human pathogens, such as
Schistosoma. A well-known authority not only
on disease-bearing snails around the world, but
on land and freshwater mollusks of Puerto Rico,
on the value of mussel distribution in tracing
stream confluence, on the biology of land and
freshwater mollusks, on medical malacology, on
paleoecology, and other subjects as well. Pro-
fessor van der Schalie published well over 110
manuscripts on his research. More complete
details on his professional activities can be
found in American Malacologists and its sequel,
the Register of American Malacologists (1986).
In the Bulletin of the American Malacological
Union for 1980, Professor van der Schalie pro-
vided an illuminating review of "Fifty years of
Malacology at the University of Michigan (1929-
1975)." Herein he summarized the outstanding
features of the "Goodrich Period (1929-1944)",
the "van der Schalie Period (1944-1977)" and the
"Highlights of the Mollusk Collections" during
those years at the Mollusk Division of the
Museum of Zoology at the University of
Michigan.
At a festschrift organized by his students, for
Professor van der Schalie in Ann Arbor in April,
1978, on the occasion of his retirement in 1977,
many tributes were presented to "Van" by
Vol. 100(4)
October 31, 1986
THE NAUTILUS 117
dozens of his students, colleagues and friends.
Of particular poignance was the careful com-
ment offered by one of Van's oldest friends and
colleagues. Professor Elmer G. Berry. Several
paragraphs from Dr. Berry's unpublished
reminiscence on that occasion, follow:
"Henry van der Schalie was born in Amster-
dam, January 8, 1907. His father died when
Henry was but an infant and his mother, in
1909, emigrated from Holland to Paterson, New
Jersey, with Henry and his two older brothers.
Circumstances necessitated Mrs. van der
Schalie to find employment to provide for
herself and the three boys, John, Herman and
Henry. She was very gifted in knitting,
crocheting and sewing in general and found
employment in a cotton factory where, among
other items, skirts were manufactured. Most
likely, all three boys worked in this plant after
school and during the summer months. Henry
was assigned to the packing department, par-
ticularly the wrapping and tying of cartons of
shirts for shipment. Anyone who has observed
Henry wrapping and tying a carton can vouch
for his adroitness from the experience gained
when he was a mere lad.
"Somewhere around 1925 Henry left Paterson
for Grand Rapids, Michigan, where he enrolled
as a student in Calvin College. Although he
majored in Zoology he also completed the pre-
medical requirements because of his indecision
regarding his future profession. The head of the
Department at Calvin College was Dr. van
Heisman, a recognized parasitologist. Henry
had been influenced by (Dr. Heisman) and began
to concentrate in the field of parasitology. His
splendid scholastic record during his under-
graduate years merited commendable recom-
mendations from his professors. Although four
universities offered him assistantships, he chose
the University of Michigan and began his work
under Dr. George R. LaRue, an outstanding
parasitologist and Chairman of the Department
of Zoology.
(After coming to Ann Arbor, Henry accepted
an assistantship in the Division of Mollusks in
the new Museum of Zoology. With some reluc-
tance, Dr. Berry reports. Dr. La Rue allowed
Henry to transfer.)
"Calvin Goodrich was the Curator of Mollusks
at that time. He had formerly been the editor of
a newspaper in Ohio, but had taken an interest
in collecting shells as a hobby. He was ac-
quainted with Dr. Bryant Walker, a highly suc-
cessful practicing lawyer in Detroit. Walker had
made an outstanding reputation as a mala-
cologist and had been appointed Honorary
Curator of Mollusks at the Museum of Zoology.
Goodrich's association with Dr. Walker brought
him in contact with A. G. Ruthven, Director of
the University Museums (later President of the
University of Michigan) and with F. M. Gaige,
Director of the Museum of Zoology. It is
reported that Goodrich asked Ruthven if he
could have a small corner in the new Museums
to "play with his shell collection." He was given a
room, but the relationship between him and the
fine Curator of Mollusks was not the best, which
subsequently resulted in the resignation of Miss
Mina Winslow. With this termination, Mr.
Goodrich was appointed Curator.
"Goodrich was a highly sensitive individual
and unquestionably realized that being ap-
pointed Curator of Mollusks at the University of
Michigan was a unique position with a (status)
equal to that of Harvard or the Philadelphia
Academy of Natural Sciences. He was not
academically trained as a scientist (and that)
caused him to develop an inferiority complex.
He had a flair for writing, especially historical or
narrative experiences such as a collecting trip,
and was a much better editor of his newspaper
than a curator of mollusks.
Elmer Berry continues: "Mr. Goodrich replied
to my application for an assistantship (at the
Museum in 1933) with a frank statement that
the Museum's budget had already been trim-
med. He advised me that the only job likely to be
open would consist of feeding animals and clean-
ing their quarters. With the severe cut of ap-
propriations, even this job might be eliminated
because of lack of funds. (In) his letter written to
me on February 2, 1933, he wrote, 'We have
been rather fortunate in the students who have
worked in this division -H.B. Baker, whose
work you are familiar with; W. J. Clench who is
now clearing up his long studies of the Physidae;
Henry van der Schalie promising to be an
authority on the Unionidae; and Alan Archer,
who already knows land shells very well and has
undertaken to straighten out the Viviparidae of
North America. It would be a pleasure to add
118 THE NAUTILUS
October 31, 1986
Vol. 100(4)
your name to this small, but excellent, company,
and my hope is that it can be brought about.'
"I shall always remember my introduction to
Ann Arbor and the Museum of Zoology. It was
terribly hot and humid, (July, 1933) but I was
impressed with the beautiful rotunda of the
Museum's building and the graceful marble
stairs leading to the second floor. That morning
I met Henry van der Schalie. He was very
friendly and about the first thing he asked was
where I was staying. When I told him, the
Allenel Hotel, he replied, 'You can't afford to
stay there very long!' Henry had been raised to
be thrifty as well as energetic. Each month a
portion of his small salary went to his mother
and the remainder paid for clothing, tuition,
books, room and board. He learned quickly that
my salary of $60 per month would necessitate
stringent budgeting because the cost of living in
Ann Arbor, even in 1933, was very high. He in-
vited me to have lunch with him, providing I
could get along on a peanut butter and jelly
sandwich, which I was happy to accept. In order
to cut expenses Henry and three other zoolo-
gists were sharing a two-room apartment just a
half-block east of the Museum Building on North
University Street. I don't know what persuasive
powers Henry exerted on his three roommates,
but by two o'clock on my first day in Ann Arbor,
I was invited to become the fifth member of this
fraternity. Henry's Dutch ancestry and home-
training instilled in him a delight in getting
things clean. Each of us had certain duties to
perform in the apartment and Henry was
assigned to cleaning the kitchen and, on alter-
nate Saturdays, the bathroom. On reciprocal
Saturdays the bathroom was to be cleaned by
Nap Curtis who lived in the west wing of the 2nd
floor. When Henry finished his assignment, the
bathroom sparkled with cleanliness. Nap, in con-
trast, considered it unnecessary to spend much
time in cleaning. As soon as Henry discovered
(Nap's) perfunctory job, a furor developed and
eventually provoked a breach of friendship be-
tween the two.
"Henry received his I'h.U. in 1934 and at the
beginning of the new fiscal year he was ap-
[)ointed Assistant Curator of Mollusks. The
American Malacological Union meetings were
scheduled to be held at Stanford University dur-
ing the summer. Coodrich, who was one of the
founders of the Union, gave his endorsement
(for Henry to attend, and present a paper on his
dissertation). I was invited to drive west with
him in his Model A Ford. It was Henry's first
trip west so we made plans to see as much as we
could in the limited time. We included Yellow-
stone, the Tetons, Great Salt Lake and planned
to do some collecting in the western canyons,
Pyramid Lake -a relic lake in Nevada, Lake
Tahoe, as well as some side trips in California.
We had a delightful trip and met many mala-
cologists for the first time, the Junius Hender-
sons, the Oldroyds, and saw a few old friends,
Stillman Berry, Allyn Smith, Leo Hertlein and
others. Best of all Henry and I got to know each
other very well and found each other's company
very compatible.
"Late in 1935 Henry became an active mem-
ber of Phi Sigma. He enjoyed the meetings and
found the members very congenial. Particularly,
he was attracted to a botanist by the name of
Annette Rudolphi. Both of them enjoyed ice
skating and taking walks through the arbore-
tum. By the spring of 1936 it was obvious to me
that this attraction had developed into a serious
romance. Walking to the Museum and back
again, or while preparing dinner or washing
dishes, the major conversation was about his
girl friend. By midsummer Henry informed me
that I had better find another place to live
because they were going to be married and
would occupy the apartment we were sharing.
The date was set for Octotier 3rd and 1 was
honored in being chosen as his best man at their
wedding.
"Goodrich retired in 1944 and Henry was ap-
pointed Curator of Mollusks. He inherited a divi-
sion rich in historical importance, perhaps the
finest collection of land and freshwater mollusks
in the country, and a top notch library. Unfor-
tunately the yearly budget had i)een reduced to
poverty level. Henry didn't remain discouraged
for very long, however, and his frugality, cou-
pled with his exploring abilities that might pro-
vide increments to purchase microsco[)es,
microtomes, establishing aquarium rooms, etc.,
not only restored the budget to its original
status, but surpassed it many times. The new
addition to the Museums Building was con-
structed and this allowed the Mollusk Division to
expand in scientific areas uniciue in malacology.
Vol. 100(4)
October 31, 1986
THE NAUTILUS 119
The Division's liigh status subsequently at-
tracted splendid investigators to receive their
advanced training in malacology at the Univer-
sity of Michigan under Henry's direction.
"I well recall two phrases Henry frequently
used, particularly when it involved a person with
whom he disagreed. He would say, "Well let me
tell you, I've got news for him!" This remark
would be followed with what he was going to do,
and he wasn't fooling! The magnificent achieve-
ments accomplished by the Mollusk Division
were due to Henry's tremendous effort and
unbelievable drive. When deeply disappointed
by a granting agency's reply to a grant request
which Henry had painstakingly made, and which
had looked promising, that stated, 'We regret to
inform you. . .' Henry, having given vent to his
feelings, would end the discussion with a grin
and a shrug of his shoulders, saying, 'Oh well,
we're having fun!' "
He meant it! An inspiring teacher and fierce
advocate for rigorous study and understanding
of mollusks, Henry van der Schalie expected a
lot from us. He expected us to be rational,
careful, committed, and to derive joy from our
dedication, as he did from his. As one of his last
students, I have treasured the great legacy of
his intellect and his spirit. I never knew "Van" to
be half-hearted about anything. He was em-
phatic, enthusiastic about whatever he was do-
ing, whether it was digging into a new research
project, encouraging a student, pursuing his
beloved mollusks in their improbable habitats,
or sharing his parenting energies with his in-
comparable wife and colleague, Annette. He
regularly doted on all the accomplishments of
his children, each of whom he and Annette
always regarded with boundless, affectionate
concern and pride.
Van had a strong environmental ethic long
before the raised consciousness of the present
era. He evinced articulate, righteous indigna-
tion whenever he perceived that human error,
indifference or greed had resulted in the
destruction of a precious habitat, or failed to
fund research, or allowed neglect of irreplace-
able museum collections. I remember his re-
counting to me his participation in a panel
discussion, along with other biologists and
lawyers, on the University of Michigan campus,
in the 1970's, on aspects of environmental law.
Van related to me his consternation with the at-
titude evinced by his colleagues, who had caved
in to sophistry and had adopted a resigned,
expedient demeanor in the discussion. Van ex-
postulated, "My God! When I think of what
(natural resources) we have squandered!" Van
insisted, rightly I think, that better laws to pro-
tect the environment could not be made in a
society where knowledgeable experts didn't
care. He believed passionately in the coupling of
the fine old values of knowledge and respon-
sibility. Van's capacity for moral outrage was
good for us all. It continues to inspire and sus-
tain us as we pursue urgent, sometimes un-
popular, environmental causes of our own.
In recent years, a visit to Manchester,
Michigan, to see Van and Annette for good
mollusk talk, in their palatial spread along the
Raisin River, was a revitalizing joy. One ambled
with them about their acres, past the huge,
burgeoning vegetable gardens Van and Annette
and their son, Arnold, were cultivating in
delighted competition with each other. One
followed them through the verdant, leafy
marshland next to the river, where Van would
pridefully point out the most recent wonders of
Annette's botanical expertise, and then to the
Raisin River itself, where, thanks to van der
Schalie effort, a number of species of Lampsilis
still maintain reproducing populations.
On such jaunts I always got a lump in my
throat. I knew again that this wonderful man,
Henry van der Schalie, lived a life of indefatig-
able personal integrity. His career spanned
almost five decades of vital research at the
University of Michigan and around the world.
More, to the end, he cared deeply about
mollusks as mollusks, about human beings as
human beings. In a glowing, over-arching way
Van cared about the lovely planet that we share.
Such jaunts invariably left me with the poignant
reminder that I shall always think of Van as a
grand model. I shall always think of Van with
admiration and love.
120 THE NAUTILUS
October 31, 1986
Vol. 100(4)
CANTHARUS MULTANGULUS NEW SUBSPECIES
GRANDANUS FROM NORTHWEST FLORIDA (BUCCINIDAE)
R. Tucker Abbott
American Malacologists, Inc.
Melbourne, Florida 32902-2255
During the last few years, members of the
Gulf Coast Shell Club in Panama City, north-
west Florida, have been very active in surveying
the marine mollusks of their area. In fact, they
have published several checklists and in 1983
issued their illustrated Seashells of Bay County
and the Gulf Coast. In 1982, Robert Granda, and
later other members, collected and sent me an
unusual form of Cantharus which I now take
pleasure in naming after its original discoverer.
Family Buccinidae Rafinesque, 1815
Genus Canthnrn.'^ Roding, 1798
Cantharus tnultangulus (Philippi, 1848)
new subspecies grandanus
Descrij)tiom.-?>\\Q\\ small, up to 28 mm in
length, fusiform, light-weight, finely but coarse-
ly sculptured, and with 6 or 7 whorls. Nuclear
whorls IV2, smooth, rounded, rapidly descend-
ing, translucent tan to clear. First 4 or 5
postnuclear whorls slightly shouldered, with 10
or 11 strong, rounded, axial ribs crossed by
FIG. 1. Canlhariix muUanifuiu.s subspecies ynmdanux
Abbott, holotype, UNNM no. 8.59096, 28.7 x 14.4 mm. FIG.
2. Cantharus multangulus multangulus (F^hilippi, 1848)
from off Shell Island, Panama City, N.W. Florida, 29.1 x
15.6 mm. Both collected by Robert Granda, 1982.
about 9 or 10 very small, irregularly-sized,
square-topped, spiral threads. On the penulti-
mate and last whorl, which is smoothly rounded,
the axial ribs are obsolete. Body whorl and short
siphonal canal with about 30 to 40 fine spiral
threads of uneven size. Columella with two
weak, oblique plicae at the base. Outer lip simple
and minutely jagged. Inside of last whorl glossy
tan and with about a dozen, smooth spiral
threads. Color of outer shell tannish brown, red-
dish or whitish yellow with numerous fine
flecks, occasional narrow spiral bands and
sparse axial flames of chocolate-brown. Oper-
culum chitinous, translucent tan, elongate-oval
and filling most of the aperture. Soft parts and
radulae not examined.
Type locality -2 to 4 feet of water, on sand
and weed bottom. Islet, V4 mi east of Black Isle,
Saint Joseph Bay, off Port St. Joe, Gulf County,
northwest Florida. Robert Granda, collector,
March 13, 1982.
Types -The holotype is deposited in U. S. Na-
tional Museum as no. 859096. Parat>']oes from
the type locality have been deposited in the
Academy of Natural Sciences of Philadelphia,
the American Museum of Natural History, N.Y.,
the Museum of Comparative Zoology at Har-
vard, and the Florida State Museum, University
of Gainesville, Florida.
Records -This moderately rare subspecies has
been collected in several places in St. Joe Bay.
Linda Brunner has also collected this subspecies
in St. Andrews Bay in nearby Bay County.
Measurements (mm.)-
length
width
Holotype
28.7
14.4
F'aratype
26.8
13.1
Paratype
26.7
14.0
i'aralype
24.0
12.1
Paratype
21.1
11.0
Paratype
21.0
11.0
Remarks-The subspecies grandanus of the
northeast Gulf of Mexico differs from the
nominate Cantharus multangulus (Philippi,
Vol. 100(4)
October 31, 1986
THE NAUTILUS 121
1848) in having a lighter-weight shell, lacking
the strong shoulder nodules on the last two
whorls, in having more numerous spiral threads,
and in being a little more elongate in propor-
tions. The variations in colors and patterns are
very similar. It is possible that these colonies in
the "Panhandle" region of Florida represent an
ecological, rather than a genetic, form.
Mr. Granda obtained two "clutches" of small,
horny egg-capsules which he found on pieces of
carapace from the horseshoe crab, Limulus. The
urn-shaped capsules, about 5x8 mm, closely
resembled those so well illustrated by D'Asaro in
his account of the capsules of CantharuH
multangulus from the same region (1986, p. 86,
figs. A-D). Very similar capsules of the
nominate species from Sanibel Island were il-
lustrated by Perry and Schwengel, 1955, pi. 50,
fig. 340.
Cantharus cancellarius (Conrad, 1846) from
the same region differs in lieing more ovoid,
having a shorter spire and in having much
stronger and fewer spiral threads. The similar
muricid, Cnlotrophon ostrearum {Conrad, 1846),
has stronger shoulder nodes and a mauve to
rosy-purple aperture. Fossil C. multangulus
from the old St. Petersburg pits have fewer
axial nodes per whorl. This grou]) of species ap-
pears to t>e largely confined to southeast United
States, the Bahamas, the north coast of Cuba
and Yucatan, Mexico.
LITERATURE CITED
D'Asaro. Charles N. 1986. Egg Capsules of Eleven Marine
Prosobranchs from Northwest Florida. BtiU. Murine Sri.
39(1): 76-91, 4 figs.
Gulf Coast Shell Club (Bob Cranda and -Jim Brunner,
editors). 1983. SeaskeLls of Bay Cininlii mtd the Gi(lfC(t(it;t.
26 pp., 96 photos, 1 map.
Perry, Louise M. and Jeanne S. Schwengel 19.5.5. Murine
Shells of the Westeiyt Coast of FUiridti. Paleont. Research
Inst.. Ithaca. 318 pp, 55 pis.
Robertson, Robert. 1957. A Study of Cantharus multaiigu-
his (Philippi) with Notes on Cantharus and Pseudo-
neptunea (Gastropoda:Buccinidae). Notulae Naturae.
Philadelphia, no. 300, pp. 1-10, 19 figs.
ON THE TAXONOMICAL STATUS OF TRITONIUM VIRIDULUM
FABRICIUS, 1780 (GASTROPODA: CANCELLARIIDAE)
Jon-Arne Sneli and Oystein Stokland
Trondhjem Biologiske Stasjon
7000 Trondheim, Norway
ABSTRACT
The taxonoviic and nomenclatorial problems associated with the species
Admete viridula (Fahricius. 1780) are discussed. The fact that the type specimens
of both Admete viridula and A. crisps. Moller, 1842 are misingfrom the Zoological
Museum in Copenhagen complicates the situation considerably as three species
are involved, Tritonium viridulum Fabricius, 1780, Defrancia viridula Moller,
1842. and D. exarata Moller. 1842. Fabricius's name is to be regarded as a nomen
dubium and that Admete couthouyi (Jay, 1839) should be used as the correct name
for that species. Mailer's D. viridula and D. exarata are both good species; but D.
viridula should probably be named Oenopota decussata (Couthouy, 1839) and D.
exarata, Propebela exarata (Moller, 1842).
The original description of Tritonium
viridulum, which was published by Fabricius in
1780 without an illustration, has commonly been
regarded as the original description of Admete
viridula auctt. The description fits the species
fairly well, and the taxonomic situation would
appear quite simple.
However, Ball (1886: 298) after having ex-
amined the holotype in the Zoological Museum
in Copenhagen, claimed that the species be-
longed to the group Bela auctt. He also found
that Defrancia viridula Moller, 1842 (Fig. 1)
122 THE NAUTILUS
October 31, 1986
Vol. 100(4)
0H:-
5 6 ^7
FIGS. 1-7. 1, Pro-pehela exarata (Moller, 1842); one of the larger specimens from the syntype-collection of Moller (Zool. nius.,
Copenhagen). 2, Propebela exarntri (Moller) as drawn by G. O. Sars. 1878. 3 and 4, A specimen of Oenuputn deccusata
(Couthouy, 1839) = Bda viriduta. from the collection of Moller (Zool. mus, Copenhagen). On the label is also written: "B.
viridula (et var. inflata) = B. deccusata Couthouy var. ventricosa". 5, Admete viriduta uctt. as drawn by G. 0. Sars, 1878. 6
and 7, Holotype of Cancellaria buccinoides Couthouy, 1838 (Reg. no. 279394 in Mus. Comp. Zool, Cambridge, Mass.). The
species is Admete couthouyi Jay, 1839.
was founded on the same specimen, and con-
cluded that it was identical with Defrancia ex-
arata Moller, 1842 (Fig. 2). Ball writes that
Morch had discovered these facts before him
and Posselt (1898: 168) confirms this by referr-
ing to a handwritten catalogue by Morch. Con-
cerning the nomenclatorial situation, Posselt
claims that the correct name o^ Admete viridula
auctt. (Fig. 3) should be Admete couthouyi Jay,
1839, because the older Cancellaria buccinoides^
(Fig. 4) of Couthouy, 1838 was described in
another genus.
All three species involved in this problem
show a great deal of variability, and Fabricius
description fits both Moller's Defrancia viridula
and Admete viridula auctt. as well. Concerning
Defrancia exarata, Posselt (1898: 168) states
that Admete crispa Moller 1842, which conmion-
ly is regarded as conspecific with A. viridula
auctt., resembles D. exarata with respect to
sculpture.
This situation could have easily been cleared
up if the type specimens in question, which were
all from Greenland, had been available, but un-
fortunately the type specimens of both
Tritonium riridulum and Admete crispa appear
to have disappeared early in this century
(Jorgen Knudsen, pers. commn.). Only one sam-
ple in the collection of the Zoological Museum in
Copenhagen could possibly be Fabricius type,
but this sample contains three specimens
whereas the original description states that
Fabricius had only one specimen available. In
the Zoological Museum in Copenhagen there are
type lots of both Mollers species Defrancia ex-
arata (Fig. 2) and D. viridula (Fig. 1). The type
Vol. 100(4)
October 31, 1986
THE NAUTILUS 123
lots of the last species contains seven syntypes
and thereby shows that Moller did not base his
description on Fabricius specimen.
None of Mollers type specimen fits very
well with Fabricius description. However,
Knipowitsch (1901) illustrates a specimen oi D.
exarata from Svalbard which rather closely
resembles Admete viridula auctt. Considering
this, and that the form caWed Admete critipa has
a sculpture like that of D. exarata, we assume
that some morphological overlap between the
species is present. Although fitting the common
forms of Admete viridula auctt. better than
those of Holler's Dejrancia exarata, Fabricius
description covers the overlapping forms, with
the exception that we never have observed D.
exarata without prominent ribs on the last
whorl as mentioned in the description. How-
ever, considering the large intraspecific varia-
tion within most species in this group it is no
wonder that Dall (1886) reduced them to
synonomy.
Moller's sample of Defrancia viridula fits
Fabricius description fairly well except that the
ribs, which are said to be straight ("costae
longitudinales") in Fabricius description, are
somewhat curved. As Moller's Defrancia
viridula, which probably is conspecific with
Pleurot.oma decussata. Couthouy, 1839, has a
large intraspecific variation like all species in
this group, Fabricius description fits both
species fairly well, and one cannot apply it to
one rather than the other.
Concerning Morch's earlier opinions as first
published by Dall (1886), there is a sample in the
Zoological Museum, University of Bergen (no.
28208) which should be mentioned. This con-
tains two dry specimens of Moller's viridula
from Greenland which are identified to "Bela
viridula M. Sars" by Morch. Michael Sars never
described any species with this name, but the
sample could indicate that Morch had Moller's
species in mind when he claimed to have dis-
covered that this and Fabricius species was
founded on the same specimen. However, this is
in contradiction to the presence of the seven
syntypes of Defrancia viridula Moller in the
Zoological Museum of Copenhagen.
Some additional information about the prob-
lems within the genus Admete may be found in
Troschel's (1866-1893) work on gastropod
radulae. Troschel investigated preserved
material of both Defrancia viridula and the
genus Admete in the Zoological Museum in
Copenhagen with respect to radular teeth. He
found the radulae in D. viridula were like those
of other species within Beta auctt., while in
Admete he found two kinds of teeth. He also
found two shell forms which he called Adm,ete
viridula (Fabricius) and A. crispa Moller accor-
ding to figures in Middendorffs (1849) work on
Russian mollusks. The shell forms corresponded
with the radular forms, which may indicate that
Troschel was correct in dividing the traditional
Admete viridula into two species.
The nomenclatorial consequences of these tax-
onomic circumstances may now be summarized.
Moller's Defrancia exarata presents no prob-
lems, and in our opinion it is best placed within
Propebela Iredale, 1918. Fabricius Tritionium
viridulum seems difficult to identify with any
species, and in our opinion it should, since the
holotype is lost, be regarded as a nomen dubium.
One could use the existence of the sample iden-
tified by Morch to attach the name to Moller's
viridula, having also the facts presented by Dall
in mind. However, since both Morch and Dall
seems to have considered that Fabricius original
specimen belonged to Propebela exarata (Moller,
1842), this argument seems somewhat dubious.
The fact that Moller founded his Defrancia
viridula on a sample of seven syntypes still pre-
sent in the Zoological Museum in Copenhagen
also contradicts the view of Morch and Dall. In
our opinion, Moller's Defrancia viridula is best
placed in Oenopota Morch, 1852, probably as a
synonym of Oenopota decussata (Couthouy,
1839).
Concerning ylrf?nete viridula auctt., the oldest
name for this species is Cancellaria buccinoides
Couthouy, 1838. This name is, however, a
primary homonym of Cancellaria buccinoides
W. Wood, 1828 and has to be rejected as there
are no strong reasons why it should be referred
to the International Commission on Zoological
Nomenclature for eventual preservation. The
next available name is Admete couthouyi Jay,
1839, which meets all demands as a correct
name for the species. The type of this is also
Couthouy 's type of buccinoides since Jay's name
was proposed as a nomen novum. An eventual
separation of Mollers Adynete crispa from A.
124 THE NAUTILUS
October 31, 1986
Vol. 100(4)
couthouyi as proposed by Troschel (1866-1893)
will not be discussed in detail, but as the type
specimen of A. crispn is lost either a neotype
should be selected or a new name should be pro-
posed and Mdller's name, A. crispa, regarded as
a nornen dubium. As MoUer never described the
radula of his species the second possibility is
probably the best.
Mr. Georg Crawford kindly corrected our
English text.
LITERATURE CITED
Couthouy, J. P. 1838. Descriptions of new species of
Mollusca and shells and remarks on several polypi found in
Massachusetts Bay. Boston Jour. Nat. Hist. 2:53-111.
1839. Monograph on the family Osteodesmacea
of Deshayes, with remarks on two species o( Patelloidea,
and descriptions of new species of marine shells, a species
of Anculotu.'i. and one of Eolis. Boston Jour. Hist.
2:129-189.
Dall, W. H. 1886. Supplementary notes on some species of
mollusks of the Bering Sea and vicinity. Proc. U. S. natn.
M«,s. 9:297-309.
Fahricius, 0. 1780. Faumi Groenliindini. Johannes Gottloli
Rolhe, Kobenhavn. 452 pp.
Iredale, T. 1918. Molluscan nomenclatural prulilems and
solutions. -No. 1. Proc. Malac. Soc. Land. 13:28-40.
Jay, J. C. 1839. A catalogue of shells in the collection of John
C. Jay, M.D., with descriptions. Ed. 3. 125 pp.
Knipowitsch, N. 1901. Ueber die in den Jahren 1899-1900
im Gebiete von Spitzbergen gesammelten recenten Mollus-
ken und Brachiopoden. Ezheg. zool. Muz. 6:435-558.
Middendorff, A. T. v. 1849. Beitrage zu einer Malacozoologia
Rossica. Abt. 2 & 3. Mem. Acad. Imper. Sci. St.-Petersb..
ser. 6. Sci. nat. 6:1-187.
Moller, H. P. C. 1842. Index Molluscorum Groenlandiae.
Naturhist. Tids.'^kr. ser. 1. 4:76-97.
Posselt, H. J. (A. S. Jensen ex.) 1898. Grondlands
brachiopoder og bloddyr. Meddr. Gronland 23:1-298.
Sars, G. O. 1878. Mollusca regionis arcticae norvegiae.
Bidrag til kundskaben oni Norges nrkliske fiiuna. A. W.
Brogger, Christiania (Oslo). 446 pp.
Trochel. F. H. 1866-1893 (cont. by J. Thiele in 1891). Das
Gebiss der Schnecken zur Begmndung einer naturlichen
Classification. Vol. 2. Nicolaische Verlags-Buchhandl.,
Berlin.
Wood, W. 1828. Index Testnceoi.Ed. 2. with the plates and
suppL, London. 188 |)p.
PISIDIUM HENSLOWANUM (SHEPPARD) IN THE
CONNECTICUT RIVER, MASSACHUSETTS (BIVALVIA: PISIDIIDAE)
Douglas G. Smith
Museum of Zoology
University of Massachusetts
Amherst, Massachusetts 01003-0027
ABSTRACT
The pisidiid dam Pisidium henslowanum ha^ been coyisidered by several
authors as an introdnced species in North America despite its discovery in
several parts of North America well away from industrial centers. The species
has been recently found in the Connecticut River in Massachusetts which is the
southeastern most record yet in North America. It is suggested that this .species is
native but locally distributed. The Connecticut River record seems also to repre-
sent the softest water in which the species has been reported in North America.
Since its first discovery in North America by
Sterki (1899), the pisidiid clam, Pisidium
henslowanum (Sheppard, 182.'j), was known on
the continent from only a small number of sites
mostly clustered in the Great Lakes and St.
Lawrence River drainages (Heard, 1961, 1962;
Ilerrington, 1962). The species is well known in
the palearctic region (Woodward, 1913; Zhadin,
1957; Ellis, 1978). Herrington (1962, 1965) and
Heard (1962) determined that P. henslowanum
was introduced into North America. Subsequent
to Herrington's (1962) and La Roccjue's (1967)
reviews of the North American distribution of
P. henslou'anum. the species was reported from
a number of localities in central and western
Canada by Harris (1973), who also documented
Vol. 100(4)
October 31, 1986
THE NAUTILUS 125
the occurrence of P. henslowanum in 7000 year
old deposits. Harris (1973) used this information
to question Herrington's (1962) and Heard's
(1962) conclusions that the species was not
native to North America. Harris (1973) also
cited Herrington's (1962) listing of a much
earlier fossil date (Pliocene-Pleistocene) for P.
supinum, then considered by Herrington a
synonym of P. henslowanum. However, subse-
quent study led Herrington (1965) to accept P.
supinum as a distinct species, thus weakening
Harris' (1973) argument. Nonetheless, Harris'
(1973) data compelled a reassessment of the in-
troduced status of P. henslowanum, yet subse-
quent studies (Burch, 1975; Clarke, 1981;
Mackie, 1981) continued to follow Herrington
(1962, 1965) and Heard (1962).
During the summer of 1985, P. henslowanmn
was collected in the Connecticut River at two
locations in Hampden County, Massachusetts.
The first collection was made in the Holyoke in-
dustrial canal complex (in direct communication
with the river) in Holyoke and the second in the
river in Longmeadow. The Holyoke collections
were first made on 1 July and repeated on 27
October. Prior to each collection the canals had
been drained for routine maintenance. A total of
98 specimens were collected, of which a series of
shells have been deposited into the Museum of
Comparative Zoology, Harvard University,
Cambridge, Massachusetts (MCZ). The remain-
ing alcohol preserved material has been placed
into the Museum of Zoology, University of
Massachusetts at Amherst. The Longmeadow
collection was made on 16 September and com-
prised a single adult specimen. Previous to these
collections the only New England records for P.
henslowanum were Lake Champlain in Vermont
(St. Lawrence River system) and Aroostook
County, Maine (Johnson, 1915). Although the
Vermont record is generally accepted in subse-
quent literature, the Maine record has not been
repeated. The Maine record was listed by
Lermond (1909) as well and was credited to
Nylander as collector and Sterki (presumably)
as the authority. A search of the pisidiid collec-
tions at the MCZ revealed no specimens of P.
henslowanum from either locality.
The Connecticut River is clearly outside the
Great Lakes and St. Lawrence River drainages
and the populations in the Connecticut River
could not have been established by recent migra-
tion. Additionally, the section of the Connec-
ticut River in Massachusetts is well above the
commercially navigable portion of the river and
it seems unlikely that the population in the
Holyoke canals has been artificially founded by
"stowaways" from Europe. As argued by Harris
(1973), this species may not be introduced in
North America. It might, however, be native
but very localized and thereby easily overlooked.
The Holyoke canal collections were made in mud
and silt sediments normally under 4.5 m of
water. The single Longmeadow specimen was
collected in .5 m of water. The species is com-
mon in the Holyoke canals, particularly along
the base of the retaining walls, and is associated
with the pisidiid species Musculium securis and
Sphaerium. striatinum and juveniles of the
unionid mussels Elliptio complanata and Ano-
donta implicata. Chemical data for the canals
(Anon., 1978, 1980) includes the following para-
meters (during July, August and September):
pH = 7.0-7.7, total alkalinity = 25-35 mg/1
(CaC03), dissolved oxygen = 5.2-10.4 mg/1,
nitrate = 0.0-0.5 mg/1, chloride = 7-35 mg/1.
The chloride values in part represent runoff of
residues of municipal operations. Chlorides in
the Longmeadow portion of the river average
about 10 mg/1 (Anon., 1978). These values com-
pare well with data given by Harris (1973) and
Okland and Kuiper (1980) except for the alkalin-
ity values. In Europe, Ellis (1978) has indicated
that P. henslowanum prefers calcium rich
waters and Harris (1973) concludes that the
presence of dissolved salts are an important
characteristic of this species' habitat. Overall,
the water of the Connecticut River is relatively
soft and has average levels of chloride salts
(Wetzel, 1975). Thus P. henslowanum can ap-
parently exist in somewhat soft water.
Specimens collected on 1 July were for the
most part larviparous (11 of 13 specimens or
84% of the sample), and the 16 September
specimen from Longmeadow was larviparous
also. Of the 27 October sample, however, only
2% (2 of 85) were larviparous though many con-
tained egg masses in the gills. These seasonal
data compare well with Holopainen and
Jonasson's (1983) findings for the presence of
brooded larvae in Danish populations.
126 THE NAUTILUS
October 31, 1986
Vol. 100(4)
Acknowledgments
I thank Alan Richmond and Jenifer Bush for
assistance in the field. I also thank D. Kenneth
Boss for allowing access to collections at the
MCZ, Harvard University.
LITERATURE CITED
Anonymous. 1978. The Connecticut River water quality
data- 1978. Massachusetts Department Environmental
Quality Engineering. Division Water Pollution Control.
Westborough, Massachusetts. 147 pp.
. 1980. Connecticut River Water Quality Data-
1980. Massachusetts Department Environmental Quality
Engineering. Division Water Pollution Control. West-
borough, Massachusetts. 60 pp.
Burch, J. B. 1975. Freshwater Sphaeriacean Clams (Mol-
lusca: Pelecypoda) of North America. Malacological Pub-
lications, Hamburg, Michigan. 96 pp.
Clarke, A. H. 1981. The Freshivaler Molluscs of Canada.
National Museums of Canada, Ottawa. 446 pp.
Ellis, A. E. 1978. British Freshwater Bivalve Mollusca.
Synopsis of the British Fauna (New Series) No. 11.
Academic Press, London. 109 pp.
Harris, S. A. 1973. Pisidium henslowanum (Sheppard) in
western Canada. The Nautilus 87:86-87.
Heard, W. H. 1961. Pisidium henslouianum (Sheppard) in
Lake Michigan. The Nautilu.^ 74:12.3.
1962. Distribution of Sphaeriidae (Pelecypoda)
in Michigan, U.S.A. Malacologia 1:139-161.
Herrington, H. B. 1962. A revision of the Sphaeriidae of
North America (Mollusca: Pelecypoda). Miscellaneous
Publications Museum of Zoology. Univ. Michigan. No. 118.
174 pp.
1965. Corrections of sphaeriid nomenclature.
The Nautilus 79:42-45.
Holopainen, L J. and P. M. Jonasson. 1983. Long-term popu-
lation dynamics and production of Pisidium (Bivalvia) in
the profundal of Lake Esrom, Denmark. Oikos 41:99-117.
Johnson, C. W. 1915. Fauna of New England 13. List of the
Mollusca. Occasional Papers Boston Society Natural
History 7(13):1-231.
Lermond, N. W. 1909. Shells of Maine. Report of the Com-
missioner of Agriculture of Maine, 1909. Pp. 217-262.
Mackie, G. L. 1981. Nearctic freshwater Sphaeriacea
(Bivalvia). Bulletin Amfrican Malacological Union for
1981: 49-52.
Okland, K. A. and J. G. J. Kuiper. 1980. Small mussels
(Sphaeriidae) in freshwater in Norway-distribution,
ecology', and relation to acidification. SNSF project, IR
61/80. Oslo-As, Norway. 85 pp.
Sterki, V. 1899. Pisidia new to our country, and new species.
The Nautilus 13:9-12.
Wetzel, R. G. 1975. Limnology. W. B. Saunders Co., Phila-
delphia. 743 pp.
Woodward, B. B. 1913. Catalogue of the British species of
Pisidium (Recent and fossil) in the collections of the
British Museum (Natural History), with notes on those of
western Europe. British Museum (Natural History), Lon-
don. 144 pp.
Zhadin, V. I. 1952. MoUusks of fresh and brackish waters of
the U.S.S.R. Zoological Institute Academy Sciences
U.S.S.R. No. 46. (1965 Israel Program Scientific Transla-
tion. 365 pp.)
PRELIMINARY OBSERVATIONS OF PREDATION ON OCEAN
QUAHAUGS, ARCTICA ISLANDICA, BY ATLANTIC WOLFFISH,
ANARHICHAS LUPUS
C. M. Hawkins and R. B. Angus
Fisheries Research Branch, Scotia-Fundy Region
Halifax Fisheries Research Laboratory
Halifax, Nova Scotia B3J 2S7
ABSTRACT
Populations of the ocean quahaug, Arctica islandica, may be siisceptable to in-
tensive grazing pressure by the Atlantic wolffish. Anarhichas lupus. In stomach
analysis of four wolffish from an inshore Nova Scotia area, 85-99% of the wet
weight contents were Arctica islandica. The number of quahaugs in the stomach
contents ranged from 3-11. These individuals were 35-86 mm. in shell length and
were 4-60 years old.
The ocean quahaug (or quahog), Arctica is-
landica (Linnaeus, 1767), is an underexploited
commercial mollusk found in coastal waters of
the south shore of Nova Scotia, Canada, and on
the Scotian Shelf (Rowell and Chaisson, 1983).
These bivalves are slow* growing (Murawski et
Vol. 100(4)
October 31, 1986
THE NAUTILUS 127
al, 1982) reaching a minimum market size of
about 51 mm (2 inches) in 13 years, and long-
lived (225 years, Ropes and Murawaski, 1983).
Since they are commercially important in the
northeast of the United States (Murawski et a/.,
1982) and are of potential commercial impor-
tance in the south shore area of Nova Scotia it is
important for the fishery biologist and manager
to assess the impact of natural predation on
stocks in relation to stock assessment and
potential yields. Quantative data on the diet of
the common Atlantic wolffish is sparce as are
data on natural predation of ocean quahaugs.
Early works (Verrill 1871, Gill 1911 and others)
are primarily qualitative but indicate that shell-
fish play an important role in wolffish nutrition.
Bowman et al. (1976) provide more quantitative
data. They examined the stomach contents of
127 wolffish from offshore waters of western
Nova Scotia. Approximately 42% of all
stomachs were empty, but the remainder on
average contained about 28% (by wet weight)
bivalves. However, no further taxonomic break-
down was made. Although there is evidence of
offshore predation of Ardica islandica by cod
{Gadus morhua) (Arntz 1974, 1978) there is a
lack of both qualitative and quantitative data
relating to predator induced natural mortality
ofArctica islandica in coastal waters. From our
investigation in the coastal waters of Nova
Scotia, Canada, qualitative and quantitative
data make the common Atlantic wolffish,
Anarhichas lupus, a prime suspect as an impor-
tant predator oi Ardica islandica.
During the first of a three year study begun in
1982 to study maturation oi Ardica islandica at
Port Mouton, Nova Scotia (64 5rN, 43 56'W)
one of us (RBA) noted the arrival of wolffish to
the study site in the spring and their departure
in late summer. The time of this annual migra-
tion corresponded to wolffish bycatches in net
and traps reported by local fishermen operating
in other areas near our study site. The fisher-
men also noted that the wolffish guts were full
of shell material. This information prompted us
to catch wolffish at our study site to determine
whether or not they were feeding on quahaugs
and, if so, their impact on known quahaug
stocks.
The study site, about 4000 m^ of flat sandy
bottom, had been surveyed 30 times with
SCUBA prior to sampling for wolffish. The area
was found to be generally void of any macro-
epibenthos commonly eaten by wolffish, i.e.
crabs, gastropods, and sea urchins (Bigelow and
Schroeder, 1953). Wolffish inhabiting this area
were collected by a diver who speared the fish
and returned to the support craft where fresh
weight {+/- 0.1 kg) overall length (+/- 0.5 cm)
and sex were recorded. Whole intact stomachs
were then removed and fixed in 10% formalin in
seawater.
In the laboratory the total weight of the
stomach contents (excluding liquids) was first
determined. Subsequently, stomach contents
were sorted and recognizable materials were
pooled prior to weighing ( + /- 0.1 g wet
weight). The number and size of quahaugs eaten
by wolffish was then determined. Recognizable
umbo portions of valves were separated from
stomach contents through careful examination
of shell fragments. The number of paired
umbones was considered representative of the
number of quahaugs eaten. The original size of
the live quahaugs eaten was determined by
matching the fragmented umbo pieces with
other valve fragments to assemble whole or par-
tial valves. Size was attained by superimposing
on the whole intact valves of a known size. Suc-
cess in assembling the valves contributed to con-
fidence in determining the numbers and sizes of
the quahaugs consumed. From previous re-
search on the biology of Ardica islandica by
Rowell and Chaisson (1983), relationships were
developed for animal size (overall length in cm)
to age and whole fresh weight to equivalent
meat weight. Estimates of the total fresh
weight as well as equivalent meat weight con-
sumed by each fish was then determined from
the number and size composition of quahaugs in
gut contents.
The general, solitary, non-schooling nature of
wolffish (Bigelow and Schroeder, 1953) is sup-
ported by our findings that few wolffish were
caught at our study site. We encountered wolf-
fish in only four of twelve SCUBA surveys over
three months of study (June 1983; May, July
1984). In addition, we noted that once a wolffish
was removed another occupied the former resi-
dence position by our return. This may indicate
that wolffish occupy and possibly defend large
territories which may exceed the 4000 m^ area
128 THE NAUTILUS
October 31, 1986
Vol. 100(4)
of our study site.
Only five woiffish were caught for stomach
content analysis (Table 1). The largest individual
measured 101.6 cm in overall length and
weighed 12.0 kg, the smallest was 72.6 cm and
4.4 kg wet weight. Four fish contained easily
identifiable quahaug shells (Arctica islandica),
comprising 85-99% of the total gut content wet
weight (Table 1). The remaining foods (1-15%)
were trace amounts of periwinkles {Littorina
sp.) sea urchins (Stronglyocentrotus droe-
hachiensis) and unidentifiable crustacean exo-
skeleton. The fifth fish was packed, to a point
where the stomach was distended, with finely
crushed tests of the sanddollar Echinarchinus
parma.
After assembling shell fragments for qualita-
tive analysis, we found from 3-11 quahaugs in
the gut contents of a single fish (Table 1). The
size of ingested quahaugs ranged from 35-86
mm in shell length, representing quahaugs ap-
proximately 4-60 years old. Qualitative
estimates of total fresh weights of quahaugs in-
gested per fish ranged from 255.5-737.7 g; meat
weights were from 81.1-155.3 g, respectively.
Meat weights expressed as a percentage of total
fish weight (Table 1) indicated that only 0.7-
2.2% of fish live weight is a food ration in the
form of quahaug meat.
It is realized that the sample size is small, but
the fact that ocean quahaugs comprised over
85% (by wet weight) of the diet of these woiffish
is of interest. This is supported by the insignifi-
cant amounts of macro-invertebrate fauna in
the stomaches of fish with quahaugs. In con-
trast, the sanddollar {E. parma) constituted
100% of the diet of one fish. This finding sup-
ported our reconnaissance of the study site
which revealed a general lack of macro-
epibenthos. These results further suggest a
possible selection preference for quahaugs by
woiffish, although other items of marginal food
value are also eaten. The slow growth oi Arctica
islandica (Murawaski et al. 1982) makes it
available to woiffish for 50-60 years after the
clam settles on the bottom. This is a long period
of potential exposure to predation by woiffish,
l)ut the duration of the life span infers low
natural mortality. This in part retlects low levels
of woiffish al)undance, their ability to locate and
capture prey as well as the clams ability to avoid
CO
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Vol. 100(4)
October 31, 1986
THE NAUTILUS 129
predation.
Under the assumption that a minimum daily
ration of only 5% body fresh weight is required
for maintenance (pers. comm. J. Castell, DFO,
Halifax, N.S.) the consumption of quahaugs by
wolffish in this study was considerably lower
than this minimum value and ranged from 0.7 to
2.2% (Table 1). This is probably a reflection of
low availability of ocean quahaugs in the study
area. Rowell and Chaisson (1983) estimated that
the mean density of ocean quahaugs in the im-
mediate study area was 3.8 m^ Over a much
larger area of commercial potential in the same
region (12 km^) they estimated a mean density
of 5.4 m\ In the study area, the results indicated
that wolffish probably prey on quahaugs equal
to the number in one m^ each day. Consequent-
ly, even in low abundance wolffish may exert
considerable impact on the commercial densities
of quahaugs. It's impact on quahaug beds in
areas suitable for commercial exploitation may
be higher but more research is needed to sup-
port such a hypothesis.
Acknowledgments
We wish to thank P. Woo, I&MP, DFO; D.
Chaisson, Bio-Atlantech; and J. Ropes, U. S.
Dept. Commer., NOAA, NMFS, Woods Hole,
Mass., for their assistance in sample collection,
analysis and manuscript review.
LITERATURE CITED
Arntz, W. E. 1974. A contribution to the feeding ecology of
juvenile cod (Gadus morhua L.) in the western Baltic.
Rapp. P.V. Reun. Cons. int. Explor. Mer. 166:13-19.
1978. The food of adult cod {Gadun morhua L.) in
the western Baltic. Meeresfarsch. 26(1977-78):60-69.
Bigelow, H. B. and W. C. Schroeder. 1953. Fishes of the
Gulf of Maine. Fish Bull. U.S. 53, 577 pp.
Bowman, R. E., R. 0. Maurer Jr. and J. Murphy. 1976.
Stomach contents of twenty-nine fish species from the five
regions in the Northeast Atlantic. Data report Northeast
Fisheries Centre, Woods Hole. Mass. Lab. Ref. No. 76-10,
37 pp.
Gill, T., 1911. Notes on the structure and habits of the wolf-
fishes. Proceedings U.S. National Museum 39(1782):
157-187.
Murawski, S. A., J. W. Ropes, and F. M. Serchuk, 1982.
Growth of the ocean quahaug, Arctica islandica. in the
Middle Atlantic Bight. Fish Bm.//.80:21-34.
Ropes, J. W. and S. A. Murawski. 1983. Maximum shell
length and longevity in ocean quahaugs, A rctica islandica.
Linne. ICES/CM. 1983/K:32, Shellfish Comm. 8pp.
Rowell, T. W. and D. R. Chaisson. 1983. Distribution and
abundance of the ocean quahaug {Arctica islandica). and
Stimpson's Surf Clam {Spisula polymyma) resource on the
Scotian Shelf. Can. Ind. Rep. Fish. Aquatic Sci. 142:v +
75 pp.
Verrill, A. E. 1871. On the food habits of some of our marine
fishes. Amer. Nat 5:397-400.
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130 THE NAUTILUS October 31, 1986 Vol. 100(4)
FRESHWATER MOLLUSKS OF THE DOMINICAN REPUBLICi
Jose D. Gomez, Mercedes Vargas and Emile A. Malek
Universidad Autonoma de Department of Tropical Medicine
Santo Domingo Tulane Medical Center
Dominican Republic New Orleans, LA 70112
ABSTRACT
A survey of the freshwater mollusks of the Dominican Republic revealed the
presence of 27 species, 2U of them, gastropods and 3 bivalves. There were 10 species
of the family Planorbidae and of these k were species o/Biomphalaria, namely, B.
glabrata, the intermediate host of Schistosoma mansoni, B. havanensis, B.
helophila, and B. straminea. The role of the latter 3 species in transmission of
schistosomiasis in the country is under investigation. Other families found were
Lymnaeidae, Physidae, Ampullariidae and Thiaridae with 2 species each, and
Ancylidae. Hydrobiidae and Pleuroceridae with 1 species each. There were 3
species of the Neritidae.
There have been only a few reports on the
freshwater mollusks of the Dominican Republic.
Probably the first was by Crosse (1891), who
listed the land and freshwater snails of the
island of Santo Domingo (Hispaniola), but the
nomenclature he used naturally does not agree
with that used today. Other writers have
reported the occurrence of the snail Bi.07nph.a-
laria glabrata (Say, 1818) in either a few or
several habitats (Ponce Pinedo, 1947; Olivier et
al., 1952; Etges and Maldonado, 1969;
Schneider et al., 1985), and still others have
listed a few freshwater mollusks associated with
B. glabrata (Gomez, 1973; Vargas and Gomez,
1976; Schneider et al., 1985). The lymnaeid in-
termediate hosts of Fasciola hepatica were
reported upon by some workers (Alvarez and
Cordeiro, 1977; Gomez et al., 1986).
In this paper we include the results of surveys
for the freshwater mollusks of the country car-
ried out for the last five years by the Institute of
Research in Bilharzia of the Autonomous Uni-
versity of Santo Domingo and by the junior
author.
Materials and Methods
Hydrographic maps were consulted to locate
•Contribution from the Institute de Investigaciones en
Bilharzia, U.A.S.D. Dominican Republic and the World
Health Organization Collaborating Center for Applied
Medical Malacology, Tulane Univer.sity.
freshwater bodies and detailed sectional
regional maps were prepared to locate the
various habitats. Identification of the specimens
was based on information from the Pan
American Health Organization (PAHO) Guide
(1968), Malek (1985), and various literature on
mollusks from the Great and Lesser Antilles.
Included in the information obtained for each
body of water was the associated fauna and
flora as well as the rainfall cycle and other
physical and chemical factors influencing the
mollusks; these data will be reported in a
separate paper.
Results
Twenty-four species of freshwater gastropods
were collected during this survey; these be-
longed to nine families (Table 1). Three species
of bivalves were also found. Among the
gastropod families there were 10 species of
Planorbidae, of which Biomphalaria helophila
(Orbigny, 1835) was the most common (31
habitats), B. glabrata. intermediate host of
Srhisto.'^oma mansoni (26 habitats), followed by
B. hnvanensis (Pfeiffer, 1839) (15 habitats), and
B. straminea (Dunker, 1848) (1 habitat). B.
helophila and B. hnvanensis are potential hosts
for S. mansoni. and B. straminea is a known
transmitter of this schistosome in South
America.
Other families encountered were Lymnaeidae,
Physidae, Ampullariidae and Thiaridae with 2
Vol. 100(4)
October 31, 1986
THE NAUTILUS 131
TABLE 1. Families and species of gastropods and their loca-
tions in the Dominican Republic.
Planorbidae
Biomphala ria glnhrnta
Hato Mayor; Santo Domingo; La Vega; San Cristobal;
Bayaguana; Haina; El Seibo; Sabana de la Mar; Guerra;
San Jose de los Llanos; San Pedro de Macoris; San Fco de
Macoris; Arenoso; Higuey; Miches; Nisibon; Constanza;
Jarabacoa; Cotui; San Rafael del Yuma; La Romana;
Ramon Santana; Santiago; Quisqueya; Nagua; El Valle.
B. havanensis
Santo Domingo; Haina; Bani; Palenque; S. J. de la
Maguana; Las Matas de Farfan; La Romana; Villa Vas-
quez; S. P. de Macoris; La Vega; Valverde; Puerto Plata;
Esperanza; Navarrete; Villa Gonzalez.
B. helophila
Santo Domingo; Haina; Valverde; Las Matas de Farfan; S.
J. de Maguana; Barahona; Cabral; Las Marias; Neyba;
Batey 4 and 5; Guerra; La Vega; Sabana Rey; Seibo; Hato
Mayor; LA, Yabiquin River; LA, Yugery River; LA, Yonu
River; Miches; Sta. Lucia Stream, Seibo; Lebron Stream.
Seibo; Pana Pana River; S.F.M., Juda River; S.F.M. El
Gran Estero; S.F.M. Arenoso; Bhona. Los Patos; Bhona,
Quarantitre River; La Vega. .Juma River; Ducantamiento
River; Neyba; La Cabirma, Neyba.
B. straminea
Los Llanos, SPM.
Helisomti trivolvis
Valverde Mao (canals in rice fields).
H. foveale
Santo Domingo, Distrito Nacional; concrete-lined foun-
tains, Centro de los Heroes; concrete-lined fountains.
Natural History Museum; Cabral Pond, Barahona.
Drepaiiotrema tucidum
Haina; S. J. Maguana; Cabral; Villa Vazquez; La Vega;
Puerto Plata; Mao; San Raf. del Yuma; Guerra; S.F.M.,
Casa de Altos; S.F.M.. La Estancia; S.F.M, El Aguacate;
S.F.M.. Arenoso.
D. cimex
Constanza; Haina; Gabon Pond, Haina; La Vega, El Ran-
chito; La Vega, La Cabulla; La Vega, Sabana Rey; Val-
verde, Guayacanes; Mao; Yerba de Guinea. Mao; Puerto
Plata; Villa Vazquez; Las Lagimas, Santiago; Moca;
Guerra, D.N.; S.F.M., Arenoso; D.N., Botanical Gardens.
D. anatinurn
D.N., Botanical Gardens; Haina; Km. 9 Aut, Duarte D.N.;
Villa Mella; Mao; S.J. de la Maguana; Cabral; Villa
Vazquez; Gabon Pond, Haina; Ranchito, L.V,; Tabagiia;
Puerto Plata; Dajabon; Moca; San R. del Yuma; Guerra;
Nisao; S.F.M., casa de Alto; San Fco. de Macoris; S.F.M.
Arenoso; S.F.M., El Gran Estero; Bonao; San Pedro de
Macoris.
D. aeruginotiiim
La Vega, El Ranchito.
Physidae
Physa cubensis
Constanza; La Vega, Gima; La Vega, Sabana Rey;
Guayacanes, Mao; Tabagua; Cerro Gordo, Mao; Los Pinos,
Mao; Haina.
P. morrnorata
D.N., Botanical Gardens; Haina; Hda. La El.strclla; Bani;
Sabana Grande de Palen(|ue; Guayacanes. Mao; Las Matas
de Farfan; Neyba, Batey 4 and .5; Biran Stream, Barahona;
Azua; Pedregal, Bani; Jarabacoa; Guayubin; Villa Vaz-
quez; La Vega; Mao; Tabagua; Puerto Plata; Moca River;
Juan Lopito, Moca; Hato Mayor; Martin Avila, LA;
Anguilla River, El Seibo; Yonu River, LA; Miches; Santa
Lucia Stream; El Seibo; Lebron Stream, Seibo; Guerra;
Don Gregorio Pond, Nisao; Nisao; San Fco. Macoris, Casa
de Alto; SFM, La Estancia; SFM, El Aguacate; SFM,
Arenoso; Juma; Bonao.
Lymnaeidae
Fossaria cubensis
D.N.. Botanical Gardens; Constanza; Haina; KM. 9 Duarte
Highway, D.N.; Sabana Grande de Palenque; Valverde;
Santiago; San J. de la Maguana; Barahona; Las Matas de
Farfan; Azua; Bani; Jarabacoa; La Vega; Esperanza, Mao;
Villa Vazquez; Hato Mayor; Miches; Seibo; San Fco de
Macoris; Bonao.
Pseudosuccinea coin mella
Quita Sueno Pond, Haina; D.N.. Botanical Gardens.
Ancylidae
Ferrissia irrorata
Mao River, Mao; D.N., Botanical Gardens; Cabral; Seibo;
San Cristobal; San Juan de la Maguana.
Thiaridae
Thiara granifera and T. tuberculntn
D.N., Botanical Gardens; La Vega; Santiago; San J. de La
Maguana; Paraiso, Bhona; Cabral; Descubierta; Las
Barias; Jimani; Neyba; Pedernales; Haina; Bani; Azua;
Jarabacoa; Guayubin; Villa Vasquez; Sabana de la Mar;
Miches; Nisibon; Seibo; Higuey; La Vega; San Pedro de
Macoris; San Fco. de Macoris; Guerra; Hato Mayor; Moca;
Dajabon; Ramon Santana; Puerto Plata; Nagua; Castillo:
Mao; Samana; Sanchez; Bayaguana; Nigua.
Ampullariidae
Marisa comuarietis
D.N., Botanical Gardens; Guerra; Bayaguana; San Pedro
de Macoris; La Vega; Jarabacoa; Nigua; Hato Mayor;
Nisibon; Valverde; Nagua.
Ampullaria glnuca
Los Llanos; D.N., Botanical Gardens; Hato Mayor.
Hydrobiidae
Pyrgophorus parvulus
D.N., Botanical Gardens.
Pleuroceridae
Goniobasis sp.
Nigua; D.N.. Botanical Gardens; Nisibon.
Neritidae
Neritina sp.; N. pmictulata: N. virgiriea
Puerto Plata; Haina; Santo Domingo; Nisibon.
species each, and Ancylidae, Hydrobiidae, and
Pleuroceridae with 1 species each. Three species
belonging to the Neritidae were encountered,
and 3 species of bivalves: Pisidium puncti-
forum. Eupera cubensis. and Anodonfa sp. The
first 2 species are sphaeriids, family Sphaeri-
idae, and the third belongs to the family
Unionidae.
132 THE NAUTILUS
October 31, 1986
Vol. 100(4)
More than one mollusk shared the habitat with
at least one other moliusi<. Thiara spp.,
however, did not occur together with B.
glabrata, but Marisa cornuarietis (Linnaeus,
1758) did inhabit the same waterbody as B.
glabrata. The flora and fauna in each habitat did
not limit the distribution of mollusks. On the
other hand, aquatic vegetation favored the oc-
currence of most of the species. However,
Thiara spp. always favored habitats with little
or no vegetation.
Discussion
Until 1972 B. glabrata occurred in a total of 1 1
habitats in the country (Vargas and Gomez,
1976), whereas we found it in 26 habitats in the
present survey, indicating an apparent continu-
ing dissemination. In addition to natural factors
which favor spreading, the movement and intro-
duction of ornamental plants in parks and other
locations have apparently contributed to the
dispersal of this medically important species. B.
haimnensis and B. helophila also show wide
distribution, possibly because of their ability to
adapt to habitats in the dry region of the coun-
try. B. glabrata has not yet invaded areas in the
south. B. havanensis and B. helophila are poten-
tial hosts of 5. mansoni, and specimens of B.
havanensis from Haiti have been infected ex-
perimentally (Michelson, 1976). Specimens of B.
helophila from Puerto Rico have also been in-
fected experimentally (Richards, 1961, 1963).
While this paper was in preparation a study by
Sodeman et al. (1985) was published in which
they collected 6 specimens only of B. straminea.
in the river Iguamo. We have had the opportuni-
ty to collect close to 1000 specimens of B.
straminea from Los Llanos, a different locality
but in the same general area of San Pedro de
Macoris. Our specimens showed the characteris-
tic features of this species (PAHO, 1968; Malek,
1985), that is, those of the shell, of the penial
complex, and corrugations on the vaginal sur-
face, but these corrugations were not distinct in
all specimens dissected. The previous known
geographical range of B. straminea was Mar-
tinique, Costa Rica, and South America (Brazil,
Venezuela, Guiana). We are at present testing
the susceptibility of our Dominican specimens to
infection with S. mansoni.
It seems that Helisoma trivolvis (Say, 1817)
was introduced and became established in the
northeast section of the country, and now oc-
curs in large numbers. However, Helisoma
foveale (Menke, 1830) is mainly encountered in
small artificial habitats, such as small pools and
fountains, indicating its possible introduction
with tropical ornamental fish. B. glabrata now
does not occur in the northeast, and competition
may have occurred between Helisoma trivolvis
and B. glabrata, as was demonstrated in the
laboratory (Malek and Malek, 1978).
There were 4 species of the genus Drepano-
trema; the first was D. lucidum (Pfeiffer, 1839)
and we believe that it is not D. hoffmani F. C.
Baker, 1940. This is because, first, our
specimens were never more than 7.5 mm in
diameter, and second, it seems that/), hoffmani
was described by F. C. Baker based on large
specimens of D. lucidum.
The lymnaeid Fossaria cuhensis (Pfeiffer,
1939) has been known to occur on the island
since the time of Crosse, and is a transmitter of
the liver fluke, Fasciola hepatica. Another lym-
naeid, Pseudosuccinea columella (Say, 1817),
was recently reported to occur in the Dominican
Republic (Gomez et al., 1986). This latter species
is an experimental host for i^. hepatica in Puerto
Rico (Leon-Dancel, 1970), and is a natural host
in Brazil (Ueta, 1980).
Thiara granifera (Lamarck, 1822) and T.
tuberculata (Muller, 1774) have in recent years
been introduced into the Dominican Republic as
well as other Caribbean islands. Their popula-
tions share the same habitats and they can be
confused morphologically, and thus are often
reported in the Caribbean literature as one
species, T. granifera. We have examined
specimens from Puerto Rico, Guadeloupe, and
Martinique and they all represent mixed popula-
tions but predominantly T. tuberculata. The
junior author expressed these views in a short
note (McCuUough and Malek, 1984). In a recent
publication (Starmuhlner, 1985), Thiara tuber-
culata was reported from Guadeloupe, Dominica
and Martinique. Starmuhlner made an error in
two of his figures; plate 8, Figures 6, 8 and 9 are
T. tuberculata, but Figure 7 and especially
Figure 10 are T. granifera. The two species can
be differentiated as follows: in T. granifera the
shell is characterized by distinct and raised axial
ribs reticulating with spiral threads. Whorls of
Vol. 100(4)
October 31, 1986
THE NAUTILUS 133
the spire are rather flat-sided; body whorl is
wide and its height is more than half of total
height of shell. In T. tuberculata the shell usual-
ly has low axial ribs and distinct and raised
spiral cords especially on body whorl; sometimes
whorls are nearly smooth with only incised
spiral threads. Whorls are evenly rounded; body
whorl is less in width than in T. granifera and its
height is less than half of shell height; the shell is
more slender than that of T. granifera. and is
uniformly turreted. The position of the brood
pouch is similar in both species, as well as the
mantle edge bearing finger-shaped fringes in
both. Alvarez and Mena Sanchez (1973) re-
ported that T. granifera had been introduced in-
to the eastern part of the Dominican Republic
and at present it has spread to other parts of the
country (Vargas et al., 1982). There may now be
biological control of B. glabrata by competition
with T. tuberculata and T. granifera. Some
habitats previously occupied by B. glabrata now
harbor only the two melaniid species. According
to Ferguson (1978), T. granifera competes suc-
cessfully with B. glabrata in Puerto Rico. In St.
Lucia, four field trials demonstrated that B.
glabr-ata was eliminated from marshes and
streams 6-22 months after the introduction of
T. granifera (Prentice, 1983).
Marisa corriuarietis. an operculate ampul-
lariid, was introduced into the Dominican
Republic by the personnel of the Health Depart-
ment in charge of the control of schistosomiasis
as a competitor of B. glabrata. because of the
encouraging result in nearby Puerto Rico (see
review by Ferguson, 1978). In our experience
the two snails now occur together in some habi-
tats in the Dominican Republic, and if M. cor-
nuarietis did succeed in biological control in
Puerto Rico this has taken place only in certain
situations, for example, small ponds and reser-
voirs.
The bivalves of the Dominican Republic have
not received much attention. Anodonta sp.
(family Unionidae) was recently introduced into
the country and is now present in the fish
{Tilapia and carp) ponds of the Ministry of
Agriculture in Nigua, close to the capital, Santo
Domingo.
The main species of freshwater mollusks of
the Dominican Republic are also present on cer-
tain other Antillean islands. In Haiti, which
shares the island of Hispaniola with the
Dominican Republic, Robart et al. (1976)
reported 16 species; in Puerto Rico, van der
Schalie (1948) reported 14 species; In
Guadeloupe, Pointier (1974) listed 21 species,
and in Martinique, Guyard and Pointier (1979)
listed 19 species. In this paper we report 27
species to be present in the Dominican Republic,
but some of these are of recent introduction.
LITERATURE CITED
Alvarez, J. M. V., and Cordero, E. T. C. 1977. Fascioliasis
bovina en la Republica Dominicana. Publ. Universidad
Autonoma S. Domingo. Vol. 224. Col. Ciencia y Tech. No.
5:1-189.
Alvarez, J. M. V., and Mena Sanchez, V. 1973. Hallazgo en
Dajabon, Republica Dominicana del caracol de agua dulce
"Thiara" spp. de importancia medica. Revista de la
Faciiltad de Ciencias Agroitomicat: y Veterinarias
2:.53-.54.
Crosse, H. 1891. Faune malacologique terrestre et fluviatile
de rile de Saint Domingue. Jour. Conrhyliol. 39:69-211.
Etges, F. J., and Maldonado, J. R. 1969. The present status
of bilharziasis in the Dominican Republic. Malacologia
9:40-41.
Ferguson, F. F. 1978. The role of biological agents in the
control of schistosome-bearing animals. Atlanta, Georgia,
U.S.A., U.S. Department of Health, Education and
Welfare, Center for Disease Control, 107 pp.
Gomez, J. 1983. Distribucion geografica del Biomphalaria
glabrata (huesped intermediario del Schistosoma mansoni)
en Republica Dominicana. Thesis for Licenciado en
Biologia, Universidad Autonoma de Santo Domingo.
Gomez, J., Vargas, M. and Malek, E. A. 1986. P-'seudosiic-
cinea columella (Lymnaeidae) in the Dominican Republic
and transmission of fascioliasis in the Caribbean region.
The Nautilus 100:66-68.
Guyard, A. and Pointier, J. P. 1979. Faune malacologique
dulcaquicole et vecteurs de la schistosome intestinale en
Martinique (Antilles Francaises). Ann. Parasitol. (Paris)
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A PREHISTORIC ABORIGINAL FRESHWATER MUSSEL ASSEMBLAGE
FROM THE DUCK RIVER IN MIDDLE TENNESSEE
Paul W. Parmalee and Walter E. Klippel
Department of Anthropology
University of Tennessee
Knoxville, TN 37996
ABSTRACT
A tofiil of 761 valves of freshwater mussels, representing a minimum of 28
species, was identified from a prehistoric ahoriginal cave site located along the
Duck River, Maury County, Tennessee. Two thirds of the mussels are Cumber-
landian forms and. as a group and based on known habitat requirements, suggest
that this stretch of the Duck River for some period between ca. 7.000 and 1,000 BP
was more shallow than at present with numerous riffles and swift current.
Recovery of numerous specimens of Pegias fabula from aboriginal sites located
along a ca. 150 km stretch of the Duck River irfects an extensive prehistoric
population of this mussel in Middle Tennessee. This prehistoric assemblage is
discussed in relation to Duck River m.ussel faunas reported over the last 60 years.
Several small rockshelters situated in the
Duck River bluffs were tested for aboriginal
occupation during archaeological survey work in
1978 in the proposed Tennessee Valley Author-
ity Columbia Reservoir area. One of these,
Cheek Bend Cave (40MU261), is located approx-
imately 13 km ESE of the city of Columbia,
Maury County (Fig. 1), and testing (three 1 x 2 m
excavation units) showed it to contain stratified
deposits of bone and shell to a depth of approxi-
Vol. 100(4)
October 31, 1986
THE NAUTILUS 135
TENNESSEE
10 20 JOk
FIG. 1. The Duck River in Middle Tennessee with the loca-
tion of Cheek Bend Cave and other aboriginal sites contain-
ing naiads discussed here.
mately 4.5 m. On the basis of the vertebrate
species composition within and among strata,
differing fill zones, and certain other
stratigraphic features, the deposit reflects two
distinct and well-defined major episodes of fill.
The top 2 m represent the Holocene stage and
contain remains of extant modern species. In
contrast, the faunal assemblage in the bottom
2 m, although it includes some species that still
inhabit the cave area, contains many such as the
prairie chicken, 13-lined ground squirrel and
pocket gopher that are now extirpated and
reflect a prairie habitat (Parmalee and Klippel,
1981) and/or a boreal environment, species such
as red-backed and yellow-cheeked voles, red
squirrel, northern flying squirrel, and arctic and
water shrews (Klippel and Parmalee, 1982).
Matrix from two additional one-meter-square
columns was removed during 1982 and 1983.
Only the vertebrate remains from the Pleisto-
cene strata have undergone preliminary iden-
tification, but all freshwater mussel valves from
the Holocene strata were removed and incor-
porated with the 1978-1979 specimens for this
study. Although terrestrial gastropods occurred
in all strata, aquatic gastropods, freshwater
mussel shells and prehistoric human artifacts
were encountered only in the Holocene strata.
Mussels were commonly used as a food resource
by prehistoric Indians in eastern North America
(Parmalee and Klippel, 1974) and in all proba-
bility most if not all of the naiads present in this
cave deposit were gathered by aboriginal groups
occupying the site.
The majority of valves were well-preserved
with some in the top two strata still retaining
remnants of the periostracum, but also a large
number of shells were broken with only portions
of the hinge line remaining. Because of this lat-
ter condition, an additional 555 valve fragments
could not be identified (Table 1). All species
determinations were made using comparative
reference specimens in the collections of the
Section of Zooarchaeology, Department of
Anthropology, University of Tennessee, Knox-
ville; all mollusk and vertebrate remains
recovered from Cheek Bend Cave are housed in
the Department of Anthropology.
The Duck River and Molluscan Studies
Interest by American malacologists in the
varied and abundant freshwater molluscan
fauna once present in most major river systems
in eastern North America began well over a cen-
tury ago. These beginning efforts centered
around taxonomy, and emphasis was placed on
describing and naming species new to science.
By the 1850s the majority of "new" species had
been described and the tendency then was to
treat the total molluscan fauna of a specific
region or river system. List of Shells Collected in
Central Tennessee by Hinkley and Marsh (1885)
is only one of many such references, but we cite
it because it provides not only a list of species
known from the Duck River (". . . the Duck River
and adjacent country at Columbia, Maury Co.")
at that time but also makes reference to the
abundance of many species and the habitat in
which they occurred. In addition, the following
description by Hinkley and Marsh (1885:2)
seems appropriate: "The Duck River, at Colum-
bia, is a pretty and rather picturesque stream,
the limestone bluffs along its banks having been
sculptured by the action of rain and frost into
various shapes, in places overhanging the water
and forming quite a cavern underneath. The
water is shallow, swift, and clear. . ." See Fig. 2.
After collecting the Duck River in 1921, 1922,
136 THE NAUTILUS
October 31, 1986
Vol. 100(4)
FIG. 2. View of the Duck River, Maury County, winter
1978-79, approximately 100 m upstream from Cheek Bend
Cave.
and 1923, Ortmann (1924) published a compre-
hensive treatment of the naiad fauna that in-
cluded 63 species and forms which he confirmed
and 7 that "should be credited to the Duck
River" based on previous published reports.
More recent studies by Isom and Yokley (1965)
and van der Schalie (1973) have pointed up the
fact that the Duck River naiad assemblage has
now been reduced by nearly one-fourth to about
45 species or forms. Completion of the Columbia
dam and reservoir will bring about the extirpa-
tion of most species in the effected stretches of
the river and will probably eliminate two
species, now known to inhabit only this locale,
from the entire river system. Ahlstedt (1981), in
a recent survey of the molluscan fauna of the
Duck River between the Normandy and Colum-
bia dams, found a drastic decline in the numbers
and abundance of species compared with earlier
surveys in 1965 and 1973. The section of the
Duck River above Columbia contains the last
known populations in that river of such species
as Quadrula intermedia and Lemiox rimosus. In
1982 TVA biologists transplanted ca. 4,000 in-
dividuals of L. rimosus into three other rivers
(and at one location in the upper Duck River
above the Normandy reservoir) in hopes of re-
establishing this endangered species in known
habitats where it once occurred. Success or
failure of this ongoing program has not yet been
fully evaluated (S.A. Ahlstedt, pers. commun.).
Cheek Bend Cave Mussel Assemblage
Although the shell was, for the most part, ex-
ceptionally well preserved, the disintegration of
the periostracum in the majority of specimens
and consequently loss of all color (including the
nacre in most) and pattern made specific iden-
tification of valves representing certain groups
(e.g. Villosa. Epioblasrna) impossible or ques-
tionable at best. For example, Ortmann (1924:
52) commented that "The males of D.
f = Dysyioyriia = Epioblasm.aJ florentina walkeri,
closely resemble those of the next species {cap-
saeformis), but they differ chiefly in color."
Shells of species as distinct as Lampsilis ovata
and Actinonaias pectorosa, when fresh, may be
impossible to distinguish when only the dorsal
portion of the valve (hinge line with lateral and
pseudocardinal teeth) is preserved -as in
archaeological or cave contexts.
Nevertheless, those specimens that could be
identified provide an interesting record of the
naiad species that inhabited the Duck River in
Middle Tennessee in prehistoric times (on which
there is no published data) and which, in turn,
reflect river conditions at the time they were
collected. Valves of Epioblasrna capsa^formis
(some of which may be E. florentina) comprised
nearly 20% of the identified naiads recovered in
the excavation units; at the time Ortmann col-
lected the Duck River at Columbia/Leftwich/
Lillard Mill/Willhoite it was "Rather abundant-
New [previously unreported] for Duck River"
(Ortmann 1924:53). Although still found in the
Duck River above Columbia, it is uncommon and
local in occurrence. We collected several dead
mature specimens below Lillard Mill that were,
unlike those from the cave, extremely large and
thick-shelled. The spike, Elliptio dilatata, most
of which were small, thin-shelled (for the
species) and compressed -suggestive of a
shallow small stream habitat - comprised about
12% of the cave naiad assemblage.
Ptychobranchus subtentum is another species
that was apparently common in the Duck River
near the cave site in prehistoric times; 107
valves (14%) were identified from the deposit. It
was evidently uncommon at Columbia/Leftwich/
Normandy when Ortmann (1924:40) made his
1921-1923 collections, reporting "Only a few
specimens found." His further comment that it
is "Most abundant in smaller streams above the
range of Ptychobranchui^ fasciolare, and this
seems to hold good also in Duck River" is of par-
Vol. 100(4)
October 31, 1986
THE NAUTILUS 137
ticular interest. This observation, coupled with
the numerous valves of P. subtentum. and other
species (e.g. Medionidus conradicus) or forms
from the cave that are indicative of a head-
waters and/or small stream habitat, suggests
that that section of the Duck River flowing in
close proximity to Cheek Bend Cave during the
mid-Holocene was smaller and more shallow
than it is today.
Another species represented in the cave
deposit (Stratum VII), namely Pegias fabula, is
also indicative of a fast-flowing, shallow, small
stream habitat. Archaeological surface collec-
tions were obtained from a Middle to Late
Archaic (ca. 7,000-4,000 BP) shell midden at the
Ervin Site (40MU147) during 1979. This pre-
historic site, situated ca. 29 km upstream from
Cheek Bend Cave in Maury County (Fig. 1), pro-
duced 15 specimens of P. fabula out of 1339
identified valves (Hofman, nd). During the
1982-1984 excavations at the Hays site
(40ML139), ca 40 km upstream from Cheek
Bend Cave in Marshall County, huge quantities
of aquatic gastropods and freshwater mussel
valves were removed from this Middle to Late
Archaic (ca. 7,000-4,000 BP) shell midden. In-
cluded among the valves of the 32 species iden-
tified from this site thus far (Turner, nd) were
104 specimens of P. fabula. Even farther
upstream, ca. 134 km above Cheek Bend Cave,
Robison (nd) identified 43 valves of P. fabula
(from a sample of 2,545 shells) from the Shofner
site (40BD55), Bedford County, a Middle
Woodland village dating ca. AD 600-500.
Archaeological sites on tributaries of the Duck
River have also produced P. fabula; one
specimen was recovered from Woodland and
one from Middle Archaic strata (266 valves iden-
tified) at the McCollum Rockshelter (40MU390)
along Fountain Creek in Maury County. Two
additional specimens (135 valves identified)
were recovered from Goatcliff Rockshelter
(40MU436) along the same Duck River tributary
in what appears to be Woodland context
(O'Hare, nd). Excavation of these rockshelters
took place during 1980-1981 . A single
specimen of P. fabula in the United States Na-
tional Museum collections ("Duck River," USNM
Lot No. 86229, catalogued Feb. 1888: Paul
Greenhall, pers. comm., April 1986) appears to
be the only documented historic record of this
naiad for the Duck River (Clarke, 1981).
In a recent paper Starnes and Starnes (1980)
report a viable population of P. fabula from the
Little South Fork Cumberland River, Kentucky,
a small fast-flowing stream ca. 20-25 m wide
with an average water depth of about 20 cm at
low river stages. Of additional interest is the
fact that the associated mussel assemblage in-
cludes P. subtenturn, P. fasciolare, E. dilatata,
M. conradicus. Villosa iris, Villosa taeniata,
Villosa vanuxemensis and Lampsilis fasciola.
Although valves of Alasmidonta viridis, Toxo-
lasyna cylindrellus and Lemiox rimosus were
not numerous in the Cheek Bend Cave deposit,
the presence of these species is also indicative of
a small stream habitat or stable stretches of
shallow riffles in somewhat larger rivers like the
Duck. Stansbery (1976) comments that "Pegias
fabula appears to be a rare Cumberlandian
species characteristic of stream conditions near,
but not quite in, the uppermost headwaters."
The three-ridge, Amblema plicata, and purple
warty-back, Cyclonaias tuberculata, are two of
the more common species inhabiting the Duck
River today. The 27 valves of A. plicata com-
prised only 3.5% of the total sample but were of
interest in that they exhibited characteristics
(small and compressed) of those inhabiting a
headwaters or small stream habitat. Only two
valves of the latter species were recovered in
the cave. Lexingtonia dolabelloides, a species
fairly well represented in the Cheek Bend Cave
naiad assemblage (ca. 6% of the identified
valves), still occurs in the Duck River, one of the
few remaining rivers still supporting viable
populations of this mussel. Quad^-ula inter-
media is another species of interest in that it
was present in the middle stretches of the Duck
River in prehistoric times (2 valves from Cheek
Bend Cave) and continued to survive until pre-
sent (Ahlstedt, 1981) but at very low population
levels. It was apparently never a common shell
in the Duck River as evidenced by the paucity of
specimens recovered at Cheek Bend Cave and at
the Hayes site where only five shells of Q. in-
termedia were identified out of a sample of
3,870 valves (Turner.nd).
Anomalous Valves
During the identification process it was
necessary to compare certain archaeological
138 THE NAUTILUS
October 31, 1986
Vol. 100 (4)
Table 1. Freshwater mussels Identified from Cheek Bend Cave. Maury County. Tenness.
Percent of each species within Strata and for Total Valves listed In parentheses {
Amblema pllcata (Say. 1817)
Three-Rld^e
Fusconala barnestana (Lea. 1838)
Tennessee Plgtoe
Lexington la dolabelloldes (Lea, 1840)
Slabslded Pearlyoussel
F. bameslana and/or L. dolabelloldes
Quadrula CvllQ(^l.ca (Say, 1817)
Rabbitsfoot
VII
13
(4.19)
5
(1.61)
10
(3.23)
2
(.65)
7
(12.28)
2
(.79)
4
(3.13)
2
(3.5)
4
(1.57)
2
(1.56)
A
(7.02)
23
(9.06)
1
(.39)
10
(7.81)
Total
Valves
27
(3.55)
13
(1.71)
47
(6.18)
3
(.39)
Quadrula InCenpedla (Conrad, 1836)
Cumberland Monkeyface
Cyclonalas tuberculata (Raflnesque, 1820)
Purple Wartyback
Elliptlo dllatata (Raflnesque. 1820)
Spike
Hemlstena lata (Raflnesque. 1820)
Cracking Pearlymussel
Pleurobema ovlforme (Conrad. 1834)
Tennessee Clubshell
Alasmldonta virldla (Raflnesque, 1820)
Slippershell
Peglas Fabula (Lea. 1836)
Llttle-wlnged Pearly Mussel
Lasaigona costata (Rafineaque, 1820)
Fluted Shell
SCrophitus undulatu!
Squawfoot
Actlnonalas pectorosa (Conrad, 1834)
Pheasant she 11
Toxolasma cyllndrellus (Lea. 1868)
Pale Lllllput
Toxolasma llvldus (Raflnesque, 1831)
Purple Lllllput
Eploblasma capsaeformls (Lea. 1834)
and /or E. fjgrentlna (Lea. 1857)
Oyster HusseT i/or Tan Rlffleshell
Eploblasma brevldens (Lea, 1834)
Cumberland Combshell
Lanpsllls fasclola (Raflnesque, 18
Wavy-rayed Lampmussel
Lampsllls ovata (Say. 1817)
Pocket book
Lemiox rimosus (Raflnesque. 1831)
Blrdwlng Pearlymussel
Medlonldus conradlcus (Lea, 1834)
Cumberland Moccasin
Potamllus alaCus (Say, 1817)
Pink Heelsplitter
1
(8.33)
(.65)
10
(3.23)
4
(1.29)
1
(.32)
2
(.65)
(.97)
1
(8.33)
17
(5.48)
1
(8.33)
5
(1.61)
4
(33.33)
49
(15.81)
1
(.32)
(3.51)
1
(1.75)
10
(17.54)
1
(.39)
1
(.78)
2
(.26)
1
(.78)
2
(.26)
43
(16.93)
9
(7.03)
90
(11.83)
1
(.39)
1
(.78)
2
(.26)
1
(.39)
4
(.53)
1
(.39)
4
(3.13)
8
(1.05)
1
(.78)
11
(1.45)
2
(1.56)
6
(.79)
1
(.13)
4
(1.57)
8
(6.25)
15
(1.97)
1
(.39)
5
(.66)
1
(.39)
(.13)
40
(15.75)
16
(12.50)
150
(19.71)
1
(.39)
1
(.13)
10
(3.94)
1
(.78)
14
(1.84)
(4.69)
23
(17.97)
13
(1.71)
100
(13.14)
Vlllosa Iris (L«a, 1830)
Rainbow
Vlllosa taenlata (Conrad. 1834)
Painted Creekshell
Vlllosa vanuxemensls (Lea, 1838)
Mountain Creekshell
Vlllosa spp. (Eploblasma?)
Ptychobranchus faaciolare (Raflnesqui
Kldneyshell
Ptychobranchus sub ten cum (Say,
Fluted Kldneyshell
17
(5.48)
(1.29)
10
(3.12)
2
(3.51)
3
(1.18)
2
(1.56)
11
(1.45)
1
(1.75)
35
(13.76)
20
(15.63)
73
(9.59)
2
(3.51)
1
(.39)
1
(.78)
8
(1.05)
1
(1.75)
8
(3,15)
4
(3.13)
24
(3.15)
1
(.39)
1
(.13)
4
(7.02)
58
(22.83)
12
(9.38)
107
(14.06)
Totals
(Identified valves)
Totals
(Unidentified valves)
(99.97)
17
310
(99.90)
57 254
(99.99) (99.96)
128 761
(100.01) (100.00)
Totals
(All Valves)
Vol. 100(4)
October 31, 1986
THE NAUTILUS 139
specimens, particularly incomplete valves and
those of Villoma spp. and Epioblnsma spp., with
fresh material using a binocular scope. Under
magnification, a variety of anomalous struc-
tures or conditions were noted that, in addition
to making specific determinations difficult or
impossible, pose some interesting questions.
These anomalies consisted primarily of deep pits
along, under and/or between the lateral and
pseudocardinal teeth and the development of
supernumerary "teeth" or projections between
or adjacent to the pseudocardinal teeth (Fig. 3).
Less than 3% of the valves exhibited one or
more of these anomalies; the majority occurred
in small, thin-shelled individuals. Possibly these
conditions were the result of some trauma or
perhaps parasites, but whatever the cause(s).
F^IG. 3. Examples of anomalous naiad valves from Cheek
Bend Cave that exhibit pitting and nacre deformities.
such abnormalities have not been observed in
other archaeological naiad material from pre-
historic sites along the Duck River.
General Discussion
Ortmann (1924:19), in attempting to evaluate
the zoogeographical affinities of the Duck River
naiad assemblage, made the following signifi-
cant observations: "Duck River being located
between Cumberland River in Kentucky and
Tennessee, and Tennessee River in northern
Alabama, might be expected to contain a similar
fauna to these two systems, a fauna which is
known to contain peculiar elements, not found
outside of this region in the Central basin
(Mississippi and Ohio drainages), which might be
called 'Cumberlandian' types (from the
'Cumberland subregion')." On the basis of his
studies of the Duck River mussel species and
those of other rivers of the southeastern region,
he concluded (Ortmann 1924:61) that "It ap-
pears that the Cumberlandian fauna is the
original fauna of Duck River, while the interior-
basin-fauna is a later invasion of the river, com-
ing up from the lower parts; yet important
elements of the interior fauna have not yet
reached Duck River. In the lower Duck, at Cen-
treville, and probably farther down, the interior
fauna alone is present, and this part does not
belong to the Cumberland region. Duck River
originally was more directly connected with the
Cumberland and Tennessee, and, at that time, it
was a rather small river." Approximately 65% of
the species represented in the Cheek Bend naiad
assemblage are Cumberlandian as defined by
Ortmann, and they reflect a headwaters or small
stream habitat. Several other species (e.g. E.
dUatata, A. plicnta) present in the cave with
Mississippian or Interior Basin affinities exhibit
small stream shell characters, that is, com-
pressed, thin-shelled small valves. Therefore,
the naiad assemblage recovered from the Cheek
Bend Cave excavations and the occurrence of
certain species such as P. fahula from this cave
and other aboriginal sites in Maury, Marshall
and Bedford counties suggest that the Duck
River in Middle Tennessee was swift and
shallow with riffles and a probable substrate of
sand and small gravel for extended periods be-
tween 7,000 and 1,000 BP.
140 THE NAUTILUS
October 31. 1986
Vol. 100(4)
Acknowledgments
We would like to express our appreciation to
Terry Faulkner for preparing Fig. 1 and to
Betty W. Creech for typing the manuscript.
Special thanks are extended to W. Miles Wright
for photographing the specimens in Fig. 3 and
the preparation of Figs. 2 and 3. We gratefully
acknowledge the Tennessee Valley Authority
under whose auspices (contracts No. TVA TV-
49244A and TVA TV-53013A) the excavation of
Cheek Bend Cave, plus the analysis of the faunal
materials recovered, were made possible.
LITERATURE CITED
Ahlstedt, S. A. 1981. The molluscan fauna of the Duck River
between Normandy and Columbia dams in central Tennes-
see. Bull. Amer. Malacol. Union for 1980. pp. 60-62.
Clarke, A. H., Jr. 1981. The Tribe Alasmidontini (Unionidae:
Anodontinae), Part I: Pegias. Alastnidonta. and Ar«rf«i.s.
Smithsonian Contributions to Zoology No. 326. 101 pp.
Hinkley, A. A. and P. Marsh. 1885. Lis? of shells collected in
central Tennessee. Published privately. Aledo, Illinois.
10 pp.
Hofman. J. L. nd. Ervin; A mid Holocene shell midden on the
Duck River in the Nashville Basin of Tennessee. Manu-
script on file, Department of Anthropology, University of
Tennessee, Knoxville, TN.
Isom, Billy G. and Paul Yokley, Jr. 1968. The mussel fauna
of Duck River in Tennessee, 1965. Airie?'ican Midland
Naturalist 80(l);34-42.
Klippel, W. E. and P. W. Parmalee. 1982. Diachronic varia-
tion in insectivores from Cheek Bend Cave and environ-
mental change in the Midsouth. Paleobiology 8(4):447-458.
O'Hare, C. R. nd. Goatcliff and McCoUum rock.shelters:
analysis of cultural and non-cultural processes operating
on the formation of two faunal samples. MA thesis in
preparation. Department of Anthropology. University of
Tennessee, Knoxville, TN.
Ortmann, A. E. 1924. The naiad-fauna of Duck River in Ten-
nessee. American Midland Naturalist 9(2): 18-62.
Parmalee, P. W. and W. E. Klippel. 1974. Freshwater
mussels as a prehistoric food resource. American Anti-
quity 39(3):421-434.
1981. A late Pleistocene population of the pocket
gopher, Geomys cf. bursarus, in the Nashville Basin, Ten-
nessee. Jour. Mammalogy 62(4):831-835.
Robison, N. D. nd. An analysis and interpretation of the
faunal remains from eight late Middle Woodland Owl
Hollow phase sites in Coffee, Franklin and Bedford coun-
ties, Tennessee. Ph.D dissertation in preparation, Depart-
ment of Anthropology, University of Tennessee, Knox-
ville, TN.
Stansbery, D. H. 1976. Status of endangered fluviatile
mollusks in central North America: Pegias fabula (Lea,
1838). Report prepared for the U.S. Department of the In-
terior, Fish & Wildlife Service and the Bureau of Sport
Fisheries & Wildlife, Washington, D.C. 8 pp.
Turner, W. B. 1984. A preliminary analysis of prehistoric
fresh-water bivalve species composition changes from ca.
7500 to 2500 B.P.: a view from the central Duck River
drainage. Manuscript on file. Department of Anthro-
pology. University of Tennessee, Knoxville, TN.
van der Schalie, H. 1973. The mollusks of the Duck River
drainage in central Tennessee. Sterkiana 52:45-56.
THE FATE OF PELECYPOD FAMILIES, SUBFAMILIES, AND TRIBES
DURING AND AFTER THE CRETACEOUS PERIOD
David Nicol
Box 14376, University Station,
Gainesville, FL 32604
ABSTRACT
Of the lU surveyed supergeneric groups of pelecypods that occur in the
Cretaceous, 38, or 33%, are extinct. In the Early Cretaceous one group became ex-
tinct every 9,300,000 years. During the Late, but not latest. Cretaceous, one group
became extinct every 2,333,000 years. In the Maastrichtian Stage (latest
Cretaceous), the extinction rate increased to one group every 470.000 years. Only
seven groups became extinct during the Cenozoic: four during the Eocene and
three during the Miocene. There was only one extinction of a supergeneric group
every 9,500,000 years during the entire Cenozoic, which is comparable to the ex-
tinction rate during the Early Cretaceous. The rate of extinction of supergeneric
groups of pelecypods increased rapidly in the Late Cretaceous and reached a
climax at the end of that geologic period.
The number of families, subfamilies, tribes
and groups of pelecypods that undoubtedly had
one or more genera living during the Cretaceous
Period, as reviewed in the Treatise on Inverte-
Vol. 100(4)
October 31, 1986
THE NAUTILUS 141
brate Paleontology (1969, 1971), is 124. In each
of these supergeneric categories the genera and
subgenera were tallied in each geologic Period
and Epoch. In a few instances, more current
data were used when it was available (Keen's,
1980, latest review of the Cardiidae), and a few
of the geologic ranges of other supergeneric
groups have been brought up to date. Ten of the
124 supergeneric groups were excluded because
of insufficient geologic data, as, for example,
the Solemyidae, Manzanellidae, Dimyidae, and
Sportellidae.
The supergeneric groups that lived during the
Cretaceous are, commonly, not ancient line-
ages. Only the Nuculanidae and Malletiidae can
be traced back to the Ordovician, and they are
as diverse today as they have ever been. Fifty
three supergeneric groups (47%) appear in the
Cretaceous. Some of these are short-lived
groups but many others first appeared in the
Cretaceous and are presently represented by
many genera and species. By the end of the
Cretaceous, most of the basic adaptive radiation
of the pelecypods had occurred. Of the 114
supergeneric categories considered herein, 90%
first appeared in the Mesozoic. Stanley's graph
(1968, p. 215) depicts the great Mesozoic
radiation.
The 114 supergeneric groups can be placed in
seven categories based on the distribution of
their genera and subgenera from the
Cretaceous to the Recent.
1. Many supergeneric groups were relatively
unaffected by the mass extinctions at the end of
the Cretaceous and remained as diverse in the
Cenozoic or increased in diversity during that
Era. In this first category there are 46 super-
generic groups or 40% of the total of 114.
Although some genera became extinct during
the Cretaceous, they were quickly replaced by
new genera arising in the Cenozoic. Almost 62%
of these supergeneric groups began in the
Cretaceous and 87% began after the Paleozoic.
Those groups first appearing in the Cretaceous
are commonly represented by one or two
genera. In other words, they are comparatively
young supergeneric groups. The protobranch
families Nuculidae, Malletiidae, and Nuculani-
dae are exceptional in that they range well back
into the Paleozoic and were not affected greatly
by extinction at the end of the Mesozoic.
2. Some supergeneric groups were affected
by Cretaceous extinction but later recovered
and became most diverse in the Neogene. There
are 15 supergeneric groups that have this
distribution in diversity, which comprise about
13% of the total. In this category only six or
40% began in the Cretaceous but 93% began in
the Mesozoic. In general, the families are longer
ranging than those that were little affected by
the Cretaceous extinctions. Some notable ex-
amples of supergeneric groups in this category
of diversity are the Pitarinae, Tellininae, Car-
diinae, Protocardiinae, and Mactrinae.
3. Some supergeneric groups were affected
by Cretaceous extinction but continued on to the
Recent with a reduction in diversity. In this
category are included 15 supergeneric groups or
approximately 13% of the total. These super-
generic groups are still longer ranging than
those in the first two categories and only four,
or 27%, began in the Cretaceous. However, 13,
or 87%, had their inception in the Mesozoic.
There are some notable groups that were
adversely affected by the Cretaceous wave of
extinction, including the Trigoniidae, which has
survived to the present only in the Australian
region. The Pholadomyidae is another group
that is nearly extinct after its great diversity in
the Mesozoic. Other relict groups at present are
the Grammatodontidae, Cucullaeidae, Fim-
briidae, and Arcticidae. All of these families
were much more diverse and widespread during
the Cretaceous.
Of the 114 supergeneric groups studied, 38, or
33% are extinct. They can be grouped into four
categories.
4. A few supergeneric groups became extinct
during the Early Cretaceous (before the
Cenomanian). There were only five families or
about 4.4% of the supergeneric groups that
became extinct during this span of time. Eighty
percent of this small group are confined to the
Mesozoic, which includes the Neomiodontidae, a
small family that lived in brackish and fresh
water.
5. There are nine supergeneric groups of
pelecypods that became extinct in the Late
Cretaceous but before the Maastrichtian. This
category constitutes 7.9% of the total number of
supergeneric groups. Four of these are small
and short-lived families and subfamilies that
14:^ THE NAUTILUS
October 31, 1986
Vol. 100(4)
were confined to the Cretaceous Period. One of
these short-lived families, the Trigonioididae,
lived in fresh and brackish water. I have placed
the Mactromyidae in this category because
Bathycorbis Iredale is most likely an aberrant
venerid and Dockery (1982, p. 72) has proved
that Cordiula Meyer was based on a young
specimen of Nemocardiurn. The Mactromyidae
is found primarily in the Jurassic and
Cretaceous.
6. Seventeen supergeneric groups, about 15%
of the total, became extinct at the end of the
Cretaceous during the Maastrichtian Stage.
Some of the supergeneric groups that became
extinct at this time were large-sized, diverse,
and common in strata of Cretaceous age. These
include the rudist families Hippuritidae,
Radiolitidae, Caprinidae, Monopleuridae, and
Requiniidae. It also includes the Inoceramidae
and Exogyrini. Seven of these seventeen groups
(41%) were confined to the Cretaceous Period,
and 14 (82%) were found only in the Mesozoic.
The great extinction at the end of the
Cretaceous did not greatly affect most of the
older supergeneric groups.
7. Seven supergeneric groups (6.1%) survived
the Cretaceous but became extinct in the Ter-
tiary-four in the Eocene and three in the
Miocene. Except for the Bakevelliidae and
Eriphylinae, they consist of small groups (no
more than four genera), and all hut the Bakevel-
liidae and Eriphylinae originated in the
Cretaceous Period. It is known that extinction
rates increased near the end of the Eocene
Epoch, as in the planktonic Foraminiferida, and
for this reason it is not surprising that a few
supergeneric groups of pelecypods disappeared
at this time. Two of the three extinctions of
supergeneric groups that occurred in the
Miocene were the Gryphaeostreinae and the
Flemingostreinae (Ostracea) and may have been
caused by oncoming glaciation at the end of the
Miocene (Nicol, 1984).
Fresh-water pelecypods were somewhat af-
fected by the Cretaceous extinctions. Besides
the two previously mentioned short-lived groups
that became extinct in the Cretaceous, the Cor-
biculidae and Unioninae lost some genera and
subgenera at the end of the Mesozoic.
In Table 1 I have summarized the rate of ex-
tinction of the supergeneric groups of pele-
TABLE 1. Extinction rates of families, subfamilies, and
tribes of pelecypods during the Cretaceous and Cenozoic.
Stratigraphic time units Number of Extinction
and time in years extinctions rate in years
1. Early Cretaceous
(Berriasian-Albian)
i.0, 500,000 5 9,300,000
2. Late but not latest
Cretaceous (Cenomanian-
Campanian) 21,000,000 9 2,333,000
3. Latest Cretaceous
(Maastrichtian) 8,000,000 17 470,000
4. Late Cretaceous
(Cenomanian-Maastrichtian)
29,000,000 20 1,115,000
5. Total Cretaceous
75,500,000 31 2,1.35,000
0, Paleocene-Eocene
30,000,000 4 7,500,000
7. Oligocene-Recent
30,500,000 3 12,170,000
3. Total Cenozoic
00,500,000 7 9,500,000
9. Total of Cretaceous
and Cenozoic 142,000,000 38 3,740,000
cypods in years throughout the Cretaceous and
Cenozoic. The actual time spans of the various
stratigraphic units were taken from Palmer,
1983. The extinction rate was low in the Early
Cretaceous, but beginning with the Cenoma-
nian, which is the earliest Stage of the Late
Cretaceous, the extinction rate increased and
continued into the Campanian Stage. This latter
rate is a fourfold increase over the Early
Cretaceous rate of extinction. The Maastrich-
tian Stage at the end of the Cretaceous has the
highest rate of extinction, being about five times
faster than the previous figure in the rest of the
Late Cretaceous, and it is about 20 times faster
than the rate in the Early Cretaceous. Further-
more, the extinction rate in all of the Late
Cretaceous was more than eight times more
rapid than it was in the Early Cretaceous. These
extinction rates do not appear to be an artifact
of the geologic record. Cretaceous strata, par-
ticularly that of a shallow-water marine environ-
ment, are exceedingly widespread and have
Vol. 100(4)
October 31, 1986
THE NAUTILUS 143
been thoroughly studied by invertebrate paleon-
tologists. Evolution increased greatly in rate
during the Late Cretaceous, a time span of
29,000,000 years. This rate of evolution in-
creased and reached a clima.\ in the latest
Cretaceous Maastrichtian Stage, which spans
only 8,000,000 years. For example, three of the
supergeneric groups that arose in the Late
Cretaceous also became extinct during that part
of the Cretaceous Period. Apparently new
species, genera, and families arose with increas-
ing rapidity during the Late Cretaceous as
evinced by the rudists (Jones and Nicol, in press,
and Nicol, in press). The Inoceramidae also
evolved rapidly during the Late Cretaceous.
One may ask, did the widespread warm shallow
seas that covered the continents during the Late
Cretaceous cause evolutionary rates to increase
greatly?
LITERATURE CITED
Dockery, D. T., III. 1982. Lower Oligocene Bivalvia of the
Vicksburg Group in Mississippi. A/).s-.s-(.s.s-(p/)) Bureau of
Geology. Bull. 123, 261 p.
Jones, D. S. and D. Nicol. Origination, survivorship, and ex-
tinction of rudist taxa. Jour. Paleontology 60:107-115.
Keen. A. M. 1980. The pelecypod family Cardiidae: A tax-
ononiic summary. Tulnne Studief: in Geology and Paleon-
tology 16:1-40.
Moore, R. C. (ed.). 1969, 1971. Treatise on Invertebrate
Paleontology. Part N, Mollusca 6, Bivalvia, Vols. 1-2
(1969). Vol. 3 (1971). Univ. Kansas Press, Lawrence, p.
N1-N1224.
Nicol, D. 1984. Critique on Stenzel's book on the Ostracea.
The Nautilus 98:123-126.
Some aspects of the evolution of the rudist pele-
cypods. The Nautilus 100(2):69-71.
Palmer, A. R. 1983. The decade of North American geology
1983 geologic time scale. Geology ll:.503-.504.
Stanley, S. M. 1968. Post-Paleozoic adaptive radiation of in-
faunal bivalve molluscs -A consequence of mantle fusion
and siphon formation. Jour. Paleontology 42:214-229.
FRESHWATER AND TERRESTRIAL SNAILS OF
SAINT LUCIA, WEST INDIES^
Emile A. Malek
Department of Tropical Medicine
Tulane University Medical Center
1430 Tulane Avenue, New Orleans, LA 70112
ABSTRACT
Surveys were made of the Jreshwater and terrestrial snails and slugs of Saint
Lucia, one of the Windward Islands of the Lesser Antilles. Ten species of 7
families of freshwater snails, 9 species of 7 families of terrestrial snails, and 2
species of one family of slugs were encountered. The freshwater snail fauna
inhabit all types of freshwater habitats available, i.e., rivers, br-ooks (ravines),
stream embankments, flood plains and swamps adjacent to rivers, drainage
ditches and ponds. Only one species of Biomphalaria, B. glabrata, was found,
although other species of this genus occur on some other neighboring islands, alone
or together with B. glabrata. The majority of the land srmil species were repre-
sented in the capital city, Castries, and the nearby hills and coastal lands. Cer-
tain species of land snails were associated with limestone deposits and others,
although inhabiting the same areas, were also found in the igneous mountain
highlands and in Jbrests. A scarcity of land operculates was observed; only one
species was found.
There is some old information on the mollus-
'Contribution from the World Health Organization Colla-
borating Center for Applied Medical Malacology, Tulane
University.
can fauna of Saint Lucia. Bland (1861), E. A.
Smith (1889, 1895) and E.A. Smith and Feilden
(1891) listed land snails and a few freshwater
snails of Saint Lucia and some neighboring
islands. The author (1965), in an abstract form.
144 THE NAUTILUS
October 31, 1986
Vol. 100 (4)
enumerated and discussed briefly the fresh-
water and land snails based on three trips to
Saint Lucia for which reports to the Pan
American Health Organization were prepared
(Malek, 1962, 1963). The snails were later
(Malek, 1980) illustrated to emphasize shell
characteristics. Jordan (1985) in a brief appen-
dix included only a short list of the freshwater
and terrestrial snails on Saint Lucia, some of
which were identified by the author.
The present report was prepared in view of
the significance of the molluscan fauna in
research on snail-transmitted diseases on the
island, especially schistosomiasis and fas-
cioliasis, and the reports in recent years on
freshwater snails in other Antillean islands such
as Guadeloupe (Pointier, 1974), Haiti (Robart et
al., 1976), Martinique (Guyard and Pointier,
1979), Guadeloupe, Dominica and Martinique
(Starmuhlner, 1985) and the Dominican
Republic (Gomez et al., 1986).
The Island of Saint Lucia
Saint Lucia, one of the Windward Islands
located between Martinique and Saint Vincent,
is a small island 27 by 14 miles and is about 233
square miles in area. The middle part is moun-
tainous; there is a longitudinal main ridge,
almost median, with other mountains running
down to the coast on either side. Between the
offshoots of the main mountain ridge are broad,
flat valleys which spread out toward the sea.
Small rivers, measuring only 7 to 12 feet in
width in most parts, and only a few feet in
depth, run from the mountain heights through
the valleys. Most rivers form separate drainage
systems that are subject to frequent flooding.
Rainfall over most of the island averages 80
inches per year, but with only 40 inches on the
southern and northern tips. The highest rainfall
occurs from May through October, with peaks in
August and September. Remnants of past
volcanic activity are still noticeable in the
sulphur area near Soufriere. The river beds have
big rocks, seemingly of volcanic origin. Also in
the geologic history certain areas were elevated,
and during the Cretaceous period, deposition of
limestone took place on several parts of the
island, which support large numbers of the
molluscan species.
Results
Ten species belonging to 7 families of
freshwater snails, 9 species belonging to 7
families of terrestrial snails, and 2 species of one
family of slugs were encountered in this survey
(Table 1). Of the freshwater snails the Planorbi-
dae was represented by 3 species, the Neritidae
by 2 species and the Lymnaeidae, Physidae, An-
TABLE 1 . Families and species of gastropods and their loca-
tions in Saint Lucia.
FRESHWATER
Planorbidae
Biomphala ria glnbrata
Rivers: Castries, in the Entrepot area; Derniere, north of
Dennery; Esperance, near Fond St. Jacques; Bance, near
bridge south of school; Choc; Raveneau, at Delcer. Brooks
(ravines): Ti Rocher; Trou Macis near Bance; above fall at
Sulphur Springs. River and brook embankments: Ravine
Poisson at Ravine Poisson; Augier River. Flood plains or
swamps off rivers: Vieu.x Fort north of Joyeox; Canaries;
Augier. Drainage ditches: Banana fields near Marquis and
in Cul de Sac Valley. Ponds: At fall near Sulphur Springs;
at Fond St. Jacques; at Derniere Fort. Concrete-lined
channels: At Ferrand Estate.
Drepanotrema depressissimum.
Pond at entrance of Union Agricultural Station; pond in
Bonne Terre area; pond in Ville Boutille; pond near
Monchy school; drainage ditch in Marquis Estate; Ti
Rocher brook; swamp by road between Vieux Fort and
Labourie.
D repanotrema I uctiiu m
Pond near Monchy school; pond in Bonne Terre area; pond
in Ville Boutille.
Lymnaeidae
Fossaria cubensis
Ditches in banana fields, Cul de Sac Valley; along bank of
river near LInion Agricultural Station; Ferrand Estate.
Physidae
Phusn ruheiisis
Derniere River; embankment along Poisson brook; Mar-
quis River; Bagatelle River in the Marchand area; pond in
Bonne Terre area; pond at Ville Boutille; pond in Monchy
area; brook joining Vieux Fort River north of Joyeax.
Ancylidae
Gundlachia radiata
Pond near Sulphur Springs; Derniere River; Castries
River in Marchand area; Choc River; ditches in banana
fields, Marquis Estate.
Hydrobiidae
Pyrgopkonis parmtlus
Brook, near Fond St. .Jacques; brook near Joyeux; brook in
Cul de Sac Valley.
Anipullaridae
Atiipulldnii ghiiica
Derniere River; Marquis River; Bonne Terre pond; pond at
entrance of Union Agricultural Station.
Neritidae
Neritina punctulata and N. virginea
Vol. 100(4)
October 31, 1986
THE NAUTILUS 145
Castries River; Marquis River; Choc River
TERRESTRIAL
Helicinidae
Helicimi fasriata
Ferrand Estate, on banana plants and weeds along drain-
age ditches.
Suceineidae
Omalonyx guadeloupensis
Banks of pond at entrance of Union Agricultural Station;
Cul de Sac Valley; along ditches in banana fields.
Succinea approximans
Along Poisson brook; along Choc River; near Vieu.x Fort;
at Union Agricultural Station.
Subulinidae
Subulina octona
Castries; Bois d'Orange; near Choc River; at Monchy; near
Union Agricultural Station.
Streptaxidae
Guletla bicolor
Castries and vicinity.
Bulimulidae
Protoglyptus aanctaeluciae
Castries and vicinity.
Bulimulus guadalupensis
Castries and vicinity; several localities along the coast and
foothills; on banana trees and shrubs in Ferrand Estate.
Urocoptidae
Brachypodella tatei
Several localities along coast and foothills
Camaenidae
Pleurodonte orbiculata
Castries; Choc River area; several localities between
Castries and northern tip of island; Bois d'Orange; Cul de
Sac Valley; Dennery.
Veronicellidae
Vaginulus occidental is
Cul de Sac Valley on banana trees; Ferrand Estate on
banana trees; hills overlooking Bois d'Orange; along
Poisson Brook.
Veroni.cella floridana
Several localities in the northern half of island, sometimes
with V. occidentalis
cylidae, Ampullaridae and Hydrobiidae by one
species each. Of the terrestrial snails the Suc-
eineidae and Bulimulidae were represented by 2
species each, while the Helicinidae, Subulinidae,
Streptaxidae, Urocoptidae and Camaenidae
were represented by one species each. Two
species of slugs found belonged to the family
Veronicellidae.
The planorbid Biomphalaria glabrata (Say,
1818), intermediate host of Schistosoma man-
soni, was found in 20 localities. Specimens,
which are up to about 10 mm in diameter, never
attain the large size of those found in Puerto
Rico, the Dominican Republic or South America.
Accordingly, F. C. Baker (1945) showed figures
of B. glabrata from Saint Lucia and commented
that they were immature. Examination of shell
features and anatomical details of biompha-
larids from various drainage systems indicated
that B. glabrata is the only species of the genus
Biomphalaria that exists on Saint Lucia. It is
known that species such as B. havanensis. B.
helophila and B. straminea occur on some of the
Lesser and Greater Antilles, alone or in addition
to B. glabrata. The snail was not found in fast-
flowing waters, but frequents and breeds on
flooded river and ravine (brook) embankments,
in swampy areas close to rivers, in side pools
and backwaters of rivers and ravines protected
by rocks and vegetation, in drainage ditches of
banana fields, and in concrete-lined channels.
Sizable colonies were always found upstream
rather than near the mouth of a river.
The planorbids Drepanotrema depressissi-
mum. (Moricand, 1839) and D. lucidum (Pfeiffer,
1839) live in ponds rich in aquatic vegetation.
The lymnaeid Fossaria cubensis (Pfeiffer, 1839)
is the snail host of Fasciola hepatica which is
common on the island. Wet mud outside the
water, with or without vegetation, represents
the typical habitat of this lymnaeid, although it
was also found in narrow drainage ditches in
banana fields, in shallow water, and in narrow
concrete-lined channels.
The Saint Lucian material of the hydrobiid
Pyrgophorus parvulus (Guilding, 1828) exhibits
variations common among individuals of this
species. Some specimens have evenly rounded
and smooth whorls, whereas other specimens
have prominent spiral carinae situated a short
distance between the sutures, and each carina
carries a number of pronounced spines.
The land snails and slugs found during the
survey seemed to be widely distributed,
especially in the island's northern two-thirds
where the tropical vegetation and coastal
deposits of limestone exist. Species such as
Subulina octona (Bruguiere, 1789), Pleurodonte
orbiculata (Ferussac, 1821), Bulimulus
guadaloupensis Bruguiere, 1792 and Protoglyp-
tus sanctaeluciae (E.A. Smith, 1889) occur in
abundance in the most populated town,
Castries. The several hills on which the town is
located and the coastal strip harbor large col-
onies of these snails. Banana plantations in
several parts of the island support large popula-
146 THE NAUTILUS
October 31, 1986
Vol. 100(4)
tions of helicinids, bulimulids, and veronicellid
slugs.
Discussion
The distribution of the freshwater snails on
Saint Lucia seems to be related to characteris-
tics of the habitat, such as the stream gradient,
water velocity, rainfall, and salinity. For exam-
ple, B. glabrata was not found in parts of
streams with steep gradients or in streams close
to the sea. The nearest colony was found at
about 400 yards from the coast. The bionomics
of S. glabrata on Saint Lucia were investigated
by Sturrock (1973, 1974). Neritina spp.,
however, seem to withstand higher salinity than
the other freshwater snails. The drepanotre-
matids were found to be almost exclusively
pond-inhabiting species, the exception being the
occurrence of Drepanotrenia depressissimum
once in a drainage ditch and once in a slow-
flowing brook.
The distribution of the land snails on this and
other Antillean islands follows the usual correla-
tion between the distribution of species and the
geological formation of the area in which they
occur. Species belonging to Brachypodella,
Gulella, and Subulina are restricted to the
limestone coastal land and adjacent hills.
Pleurodonte orbiculata (Ferussac, 1821),
Bulimulus guadaloupensis (Bruguiere, 1792),
and Protoglyptus sanctaeluciae (E.A. Smith,
1889) also inhabit these areas, but they are addi-
tionally found in the igneous mountains in the
highlands.
The main species of freshwater and terrestrial
snails on Saint Lucia also occur on certain other
Caribbean islands. The faunal relationship of
Saint Lucia to other Caribbean islands and to
the mainland in Central and South America
deserves comment. Several theories have been
postulated to explain the faunal and floral
similarities among the islands of the West Indies
on the one hand and among those of the islands
and the fauna and flora of Central and South
America on the other hand. Among the theories
postulated is the past existence of land l)ridges
(Ihering, 1931), or isthmian links (Schuchert,
1935) between the islands themselves and be-
tween the islands and the mainland of Central
and South America. Snails have played an im-
portant part in helping to correlate the geo-
logical history and the zoogeography of the
islands. Certain species, however, such as the
cosmopolitan Subulina spp. and others are of lit-
tle value in providing evidence of previous land
connections. The land operculate snails offer
evidence of zonal grouping within the West
Indies. Surveys on Saint Lucia revealed the
presence of only one land operculate, Helicina
fasciata Lamarck, 1818-1822. Thompson (1967)
described another operculate from Saint Lucia,
Lifhacaspis xanthoglauca (family Cyclophori-
dae). In general, however, there is a scarcity of
land operculate snails on the Lesser Antillean
islands and South America as compared to a
preponderance of land operculates on the
Greater Antilles islands.
Among the freshwater snails, the planorbids
show relationships with the South American
fauna. Drepanotrem.a depressissimum (Mori-
cand, 1839) is typically South American. B.
glabrata is found on some islands of both the
Lesser and the Greater Antilles, and its range
extends into South America. In the Antilles, B.
glabrata occurs on Saint Lucia, Martinique,
Guadeloupe, St. Kitts, Antigua, Dominica,
Hispaniola, and Puerto Rico. Ampullaria glauca
(Linnaeus, 1758) is also South American.
The melaniid Thiara granifera (Lamarck,
1822) was introduced by Prentice (1983) in field
trials in marshes and streams for experiments
on biological control oiB. glabrata. Whether T.
granifera still exists in these habitats or has
spread to other habitats in Saint Lucia is not
known. Jordan (1985) listed the sphaeriid
l)ivalve Pisidium punctiferum (Guppy) as a
member of the freshwater fauna of the island,
but it was not encountered in my surveys. How-
ever, his list did not include the terrestrial oper-
culate Helicina fasciata Lamarck, nor the slug
Veronicella floridana (Leidy) which were both
common in the material that I collected.
LITERATURE CITED
Baker, F. C. 1945. TheMolluncan Family Planorhidar. I'ni-
versity of Illinois Press, Urbana, Illinois.
Gomez, J. D., Vargas, M., and Malek. E, A. 1986. Fresh-
water mollusks of the Dominican Republic. The Niiittilus
100 (in press).
(Uiyani, A. and Pointier, J. P. 1979. Faune malacolofjique
diiicaquicole et vecteurs de la schistosome intestinale en
Martinique (Antilles Francaises). Ann. Pnra.'^itol. (Paris):
54: 193-205.
Vol. 100(4)
October 31, 1986
THE NAUTILUS 147
Ihering, H. von. 1931. Land bridges across the Atlantic and
Pacific Oceans during the Kainozoic era. Quart. J. Geol.
Soc. London 87:376-391.
Jordan, P. 1985. Schistosomiasis. The St. Lucia Project.
Cambridge University Press, Cambridge.
Malel<. E. A. 1962. Report on precontrol studies of bil-
harziasis in St. Lucia. Unpublished Document, Pan
American Health Organization, Washington, D.C.: 1-18.
1963. Report on a precontrol survey of bil-
harziasis in a pilot study area of St. Lucia. Second visit.
Unpublished Document, AMRO-1.55, Pan American
Health Organization, Washington, D.C.: 1-9.
. 1965. Freshwater and land snails of St. Lucia,
the West Indies. Amer. Malacot. Union. Annual Report.
p. 38.
1980. Snail-Tra7isntitted Parasitic Diseases.
Vol. I. CRC Press, Boca Raton, Florida.
Pointier, J. P. 1974. Faune malacologique dulcaquicole de
I'ile de la Guadeloupe (Antilles Francaises). Bull. Mus.
Hist. Natur.. Paris, 3rd Ser., No. 235, Zool., 159:905-933.
Prentice, M. A. 1983. Displacement of Biomphalaria
glabrata by the snail Thiara granifera in field habitats in
St. Lucia, West Indies. Ann. Trap. Med. Parasitol.
77:51-59.
Robart, G., Mandahl-Barth, G. and Ripert, C. 1976. Inven-
taire, repartition geographique et ecologie des mollusques
dulcaquicoles d'Haiti (Carabes). Hnliotts 8:159-171.
Schuchert, C. 1935. Historical Geology of the Antillean-
Caribbean Region. John Wiley & Sons, Inc., New York.
Smith, E. A. 1889. On the Mollusca collected by Mr. G. A.
Ramage in the Lesser Antiles. Report III. Ann. Mag.
Natur. Hist. (6th Ser.) 3:400-405.
1895. Report on the land and freshwater shells
collected by Mr. H. H. Smith at St. Vincent, Grenada and
other neighboring islands. Proc. Malacol. Soc. London
1:300-322.
Smith, E. A. and Feilden, H. W. 1891. A list of the land and
freshwater shells of Barbados. Ann. Mag. Natur. Hist.
(6th Ser.) 5:247-257.
Starmuhlner, F. 1985. Erstfunde von drei Arten von Suss-
wasser Gastropoden auf den Inseln Guadeloupe, Dominica
und Martinique (Kleine Antillen). Heldia 1:55-58.
Sturrock, R. F. 1973. Field studies on the transmission of
Schistosoma mansoni and on the bionomics of its inter-
mediate host, Biomphalaria glabrata, on St. Lucia, West
Indies. Int. Jour. Parasitol. 3:175-194.
. 1974. Ecological notes on habitats of the fresh-
water snail Biomphalaria glabrata, intermediate host of
Schistosoma mansoni, on St. Lucia, West Indies. Carib-
bean Jour. Sci. 14:149-161.
Thompson, F. G. 1967. A new cyclophorid land snail from
the West Indies (Prosobranchia) and the discussion of a
new subfamily. Proc. Biol. Soc. Washington 80:13-18.
ON THE REDISCOVERY OF TERAMACHIA MIRABILIS
(CLENCH AND AGUAYO, 1941), AND ITS
RELATIONSHIP TO OTHER CALLIOTECTINE VOLUTES
William K. Emerson and Walter E. Sage III
Department of Invertebrates
American Museum of Natural History
New York, N. Y. 10024
ABSTRACT
A second known specimen o/Teramachia mirabilis (Cleyich and Aguayo, 19Jfl) is
here recorded from, deep water (UGS.U meters) on the Little Bahama Bank. Com-
parisons of this dead-collected, crabbed speciynen are jnade with illustrations and
descriptions of the holotype, which was live-taken in 521.3 meters off Matayizas,
Cuba, in 1939. Largely on the similarity of shell characteristics, this New World
species is retained in the genus Teramachia, as is Calliotectum fischeri Olsson,
1964, from the Pliocene of Ecuador. Examination of the typological specimens of
Calliotectum vernicosum Dall, 1890, for which a lectotype is here designated, con-
firms the distinction between Calliotectum Dall, 1890 and Teramachia Kuroda,
1931.
Zoogeographically, Teramachia is confined mostly to the western Pacific and is
known to date froyn the Neogene of Japan as ivell as Ecuador. Thus the widely
148 THE NAUTILUS
October 31, 1986
Vol. 100(4)
separated ynodem distributional pattern of the genus Teramachia (six species in
the western Pacific, one in the western A tlantic) suggests that T. mirabilis is a sur-
viving element of a presently disjunct Pacific fauna.
Howellia mirabilis Clench and Aguayo, (1941,
pp. 177-178, pi. 14, fig. 2; Weaver and duPont,
1970, p. 178, pi. 76 A, B) was described on the
basis of a single, live-collected specimen
dredged at Atlantis Station No. 3483, off
Matanzas. Matanzas Province, Cuba (23°12'N,
81°23'W), in 521.3 meters. The soft parts unfor-
tunately were not recovered in a condition that
could be preserved, and the shell was cleaned
and dried during the trip. Regrettably, the
holotype (catalog #135291) cannot be located in
the collection of the Museum of Comparative
Zoology and is presumed lost (teste D. Backus).
This taxon was proposed as the type species for
the monotypic genus Howellia by Clench and
Aguayo (1941, p. 177). Howellia was placed pro-
visionally by Clench and Aguayo (op. cit.) in the
family Fasciolariidae, in the absence of know-
ledge of the radula and soft-part anatomy. Sub-
sequently, Clench and Turner (1964, p. 177)
assigned Howellia to the Volutidae, subfamily
Calliotectinae, following the placement of
Pilsbry and Olsson (1954, p. 19), based on shell
characters. Clench and Turner (1964, p. 178),
however, noted the resemblance in shell mor-
phology of Howellia mirabilis to the western
Pacific genus Teramachia Kuroda, 1931. Later
Weaver and duPont (1970, p. 176) placed
Howellia, 1941, in the synonymy of Teramachia,
1931, where it was retained by Emerson (1985,
pp. 102, 103).
Recently Harry G. Lee of Jacksonville,
Florida kindly called our attention to a crabbed
specimen of Teramachia mirabilis in the collec-
tion of the Indian River Coastal Zone Museum
(IRCZM) at Harbor Branch Oceanographic In-
stitution, Inc., Fort Pierce, Florida. This
specimen, apparently only the second known for
this taxon, was found in a sediment sample col-
lected on a Johnson-Sea-Link I submersible dive
during R/V Johnson Cruise 159, on October 4,
1983. The bucket had been left on the bottom for
408 days to collect accumulating sediment near
Black Rock, Little Bahama Bank (26°16.5'N,
77°38.5'W) in 465.4 meters, by C. M. Hoskin
and J. K. Reed. The specimen presumably was
carried into the 20-liter plastic bucket by the
hermit crab occupying the shell.
Although long-dead and now discolored from
the muddy sediment, this specimen, IRCZM
#065:02138 (figs. 5, 6), compares favorably with
the description and illustration of the holotype.
The present specimen is larger (125 vs. 93 mm
in height) and has weaker axial sculpture on the
body whorl. In outline and in the development of
axial sculpture on the body whorl Teranfiachia
mirabilis most closely resembles the western
Pacific Teramachia johnsoni (Bartsch, 1942, p.
12, pi. 2, fig. 3; holotype illustrated in color by
Weaver and duPont, 1970, pi. 750, H; cf. figs. 5,
6 with figs. 7, 8 herein). Teramachia johnsoni,
however, has a tannish brown shell with a
darker aperture, whereas the holotype of Tera-
machia mirabilis is whitish and tinged with a
faint brownish red. The aperture is light brown-
ish red within.
The discovery of the newly recognized speci-
men of Teramachia mirabilis extends the
known provenance of this species northwest-
ward from the vicinity of Cay Sal Bank, off
northern Cuba, to the Little Bahama Bank.
Specimens can be expected to occur at suitable
depths elsewhere on these and other regional
banks.
In the absence of anatomical data on the type
species of Howellia it seems prudent to refer
this New World species to the genus Tera-
machia on the basis of shell characters held in
common with the western Pacific species of this
group of calliotectine volutes (Weaver and
duPont, 1970, p. 177, Emerson, 1985, p. 103). A
more precise systematic assessment oi Howellia
must await knowledge of the soft parts and
radular characters of Teraynachia mirabilis.
Clench and Turner (1964, p. 178) briefly noted
the close resemblance of the shell morphology of
Howellia mirabilis to that of the Japanese
species of Teramachia, and they stated, "Rela-
tionships of this sort from widely separated
areas are unusual, but they do exist". Shortly
thereafter, Olsson (1964, p'. 129, pi. 23, fig. 4)
described Calliotectum fischeri from late
Pliocene rocks of the Esmeraldas formation of
Ecuador. The holotype is based on a 52.8 mm
Vol. 100(4)
October 31, 1986
THE NAUTILUS 149
150 THE NAUTILUS
October 31, 1986
Vol. 100(4)
fragmental specimen, which was estimated to be
"between six and eight inches in length" before
the badly fractured specimen was extracted
from the matrix. Olsson compared his specimen
to Prodallia dalli Bartsch, 1942 from the Philip-
pines and he referred Teramachia Kuroda, 1931
and Prodallia Bartsch, 1942 to the synonymy of
Calliotectum Dall, 1890. We have examined the
holotype and six fragmental specimens of
Olsson's "Calliotectum" fischeri from near the
type locality (Tulane Geol. Dept. localities 1397
[figs. 3, 4, herein] and 1402, and W. D. Pitt Coll.
locality 9A-B3-915, all from the Esmeraldas for-
mation). These specimens are from a deep-water
facies and confirm the allocation of Olsson's
taxon to the genus Teramachia. The only other
known extinct species of Teramachia was
described from the Mio-Pliocene [?Pliocene]
Shimajiri formation of Okinawa, Japan as T.
shinzatoensis (MacNeil, 1961, p. 96, pi. 9, fig. 1;
Rehder, 1972, p. 9, figs. 5, 6). It was compared
by the describer and Dr. Rehder with T.
johnsoni (Bartsch, 1942).
The placement by Olsson (1964, p. 128) of his
Pliocene Ecuadorian fossil (Teramachia
fischeri) in the monotypic genus Calliotectum
Dall (1890, p. 304) requires comment. Dall
(1890, p. 305, pi. 5, fig. 8) considered the type
species of Calliotectum (C. vernicosmn Dall,
1890) to be pleurotomoid, but he noted the shell
lacked an anal notch and a fasciole. Subsequent-
ly, Pilsbry and Olsson (1954, p. 19, fig. 16, rachi-
dian tooth) proposed the volutid subfamily
Calliotectinae with Calliotectum the type genus,
on the basis of shell and radular characters, the
radular ribbon being uniserial with a tricuspid
rachidian tooth. Pilsbry and Olsson (1954, op.
cit.) also referred Teramachia Kuroda, 1931,
with Prodallia Bartsch, 1942 as junior
synonym, to Calliotectinae. Weaver and duPont
(1970, pp. 175, 176) added Howellia Clench and
Aguayo, 1941 to the synonymy of Teramachia,
1931.
Dall (1890, p. 305) based Calliotectum ver-
nicosum on five specimens dredged by the
"Albatross", in 1888. Three of these were taken
at station 2807, in 1485 meters from the type
locality near the Galapagos Islands (00°24'00"S,
89°06'00"W). From this lot are Dall's figured
specimen USNM #96555 (1890, pi. 5, fig. 8;
Abbott and Dance, 1982, p. 224) here selected as
lectotype (figs. 9, 10), and two paralectotypes:
USNM #633904, and DMNH #10135 (Weaver
and duPont, 1970, pi. 75, A, B) - both ex USNM
#96555. The two remaining paralectotypes
(USNM #97068) were dredged at station 2793,
in 1355 meters off the coast of Ecuador
(01°03'00"N, 18°15'00"W).
These typological specimens are very thin-
shelled, with inflated whorls, the largest
specimen being the lectotype with a height of
47.5 mm (spire incomplete) and with 6V2 post-
nuclear whorls, and the smallest paralectotype
being 24.8 mm in height (spire incomplete) with
5 postnuclear whorls. Although superficially
resembling the shells of Teramachia. specimens
of Calliotectum. of the same stage of growth
FIGS. 9, 10. Calliotectum reniira^um Dall. 1890, near the
GalapaKos Islands, in 1485 meters, lectotype USNM #96555;
X 1.
FIGS. 1,2. T. dalli daydoni Poppe, 1986, off Port Hedland, northwestern Australia, in 450 meters, AMNH #221239. FIGS. 3,
4. Teramachia fifickeri (Olsson, 1964), Quebrada Camerones, Province of Esmeraldas, Ecuador, Tulane Geol. Dept. loc. 1397,
Pliocene (early whorls and basal whorls missing). FIGS. 5, 6. T. mirabilis (Clench and Aguayo, 1941), Little Bahama Bank, in
465 meters, IRCZM #065:02138. FIGS. 7, 8. T. johnsoni (Bartsch, 1942), off Panglao, Bohol. Philippines, in 365 meters,
AMNH #219986. FIGS. 1-8, approximately x 1.
Vol. 100(4)
October 31, 1986
THE NAUTILUS 151
have expanded, bulbous whorls and appear to
represent a separate calliotectine lineage (cf.
figs. 9, 10 with figs 1, 2 and figs. 3, 4). Therefore
we reject Olsson's placement of Teramachia
Kuroda, 1931 and Prodallia Bartsch, 1942 in
the synonymy of Calliotectum Dall, 1890.
The widely disjunct modern distributional pat-
tern of Teramachia, six species in the western
Pacific and one in the western Atlantic (Emer-
son, 1985; Bouchet, 1986; Poppe, 1986), with ex-
tinct species in the Mio-Pliocene of Okinawa and
the Pliocene of Ecuador, presents some prob-
lems in zoogeographic interpretation. The dis-
tribution of these deep-water mollusks is poorly
known and the genus may be of wider occur-
rence than the available data suggest. Within
the past few months, Teramachia dalli claydoni
Poppe (1986) was described from the continen-
tal slope of northwestern Australia and an ap-
parently new species of Teramachia inhabiting
deep water off New Caledonia was reported
(Bouchet, 1986). Additional species may even-
tually be found living in the eastern Pacific and
elsewhere in the Atlantic Basin. The presence of
Teramachia mirabilis living in the western
Atlantic, however, may be an example of a
Pacific faunal element which survived after
being carried into the Caribbean region on the
East-Pacific-Caribbean plate to its present posi-
tion adjacent to Cuba (see Durham, 1985). Ac-
cording to Sykes et al. (1982), the Caribbean
plate has moved east-northeast about 1,400 km
since late Eocene time. Perhaps the precursors
of T. mirabilis were carried into the western
Atlantic on this plate. Durham (1985) cites addi-
tional examples of Pacific faunal elements that
apparently moved with this plate into the Carib-
bean area.
Acknowledgments
In addition to Dr. Harry Lee, we thank Paula
Mikkelsen, Indian River Coastal Zone Museum,
Harbor Branch Oceanographic Institution, Inc.,
Fort Pierce, Florida, William D. Pitt, Sacra-
mento, California, Drs. Emily and Harold
Yokes, Tulane University, and Drs. Richard S.
Houbrick and Thomas D. Waller, National
Museum of Natural History, Smithsonian In-
stitution, for the loan of specimens in their care.
We also thank Drs. Joel Cracraft, Leslie F.
Marcus, Malcolm McKenna, and Richard H.
Tedford for an exchange of views on the bio-
geographical significance of Caribbean plate
tectonics.
We are indebted to our colleagues in the De-
partment of Invertebrates, American Museum
of Natural History for their contributions to this
study: Stephen M. Butler for the photography
and Stephanie Crooms for word-processing the
manuscript.
LITERATURE CITED
Abbott, R. T. and Dance, S. P. 1982. Compendium, of Sea-
shells. New York, 411 pp., illus. in color.
Bartsch, P. 1942. Some deep-sea Philippine volutids. The
Nautilus 56(1):9-13, pi. 2.
Bouchet. P. 1986. Oceanographic campaigns in New Cale-
donia. Rossiniana, Bull. L'Assoc. Conchyl. De Nouvelle-
Caledonie 31;3-8, illus.
Clench, W. J. and Aguayo, C. G. 1941. Notes and descrip-
tions of new deep-water Mollusca obtained by the
Harvard-Havana Expedition off the coast of Cuba. IV.
Mem. Soc. Cubana Hist. Nat. 15(2):177-180, pi. 14,
Clench, W. J. and Turner, R. D. 1964. The subfamilies Volu-
tinae, Zidoninae, Odontocymbiolinae, and Calliotectinae in
the western Atlantic. Johnsonia 4(43):129-180, pis.
80-114.
Dall, W. H. 1890 [1889]. Scientific results of explorations by
U. S. Fish Commission Steamer Albatross. VII. Prelimi-
nary report on the collection of Mollusca and Brachiopoda
obtained in 1887-'88. Proc. U. S. Nat. Mu.s. 12(737):
219-362. pis. 5-14.
Durham, J. W. 1985. Movement of the Caribbean plate and
its importance for biogeography in the Caribbean. Geology
13(2):123-125, 2 figs.
Emerson, William K. 1985. Teramachia dupreyae new
species, from off Western Australia (Gastropoda: Voluti-
dae). The Nautilus 99(4):102-107, 8 figs.
Kuroda, T. 1931. Two new species of Volutacea. Venus 3(1):
45-49, 3 figs.
Olsson, A. A. 1964. Neogene mollusks from northwestern
Ecuador. Paleont. Res. Inst., 256 pp. 36 pis,
MacNeil, F. S. 1961. Tertiary and Quaternary gastropods of
Okinawa. U. S. Geol. Surv. Prof. Paper 339 ("I960"): i-iv
+ 1-148, pis. 1-19 (distributed March 17, 1961).
Pilsbry, H. A. and Olsson, A. A. 1954. Systems of the
Volutidae. Bull. Amer. Paleont. 35(152):271-306, pis.
2.5-28.
Poppe, G. 1986. A novel species and a novel subspecies of
Volutidae from northwestern Australia. .4 pfx. Inform. Sci.
Soc. Beige de Malac. l(l):27-36, pis. 1-3.
Rehder. H. A. 1972. Some notes on the genus Teramachia
Volutidae: Calliotectinae). The Veliger 15(1):7-10, figs.
1-7.
Sykes, L. R., McCann, W. R., and Kafka, A. L. 1982. Motion
of Caribbean plate during last 7 million years and implica-
tions for earlier Cenozoic movements. Jour. Geophysical
Res. 87(B13):106.56-10676.
Weaver. C. S. and duPont, J. E. 1970. Living Volutes: a
monograph of Recent Volutidae of the world. Delaware
Mus. Nat. Hist. Mong. Ser., No. 1, xv + 375 pp., 79 col.
pis., 44 figs., 13 maps.
152 THE NAUTILUS
October 31, 1986
Vol. 100(4)
REMINISCENCES
[About a hundred years ago The Nautilus published many anecdotal accounts,
but as the journal became more technical there was rarely an opportunity to add a
personal touch. Because this 100th anniversary volume is dedicated to mala-
cologists who have contributed in the past, we are including a few personal
reminiscences by friends of William J. Clench and Joseph Rosewater. To the list
of departed fellow-malacologists we regretably must add the name of that
distinguished freshwater expert, Henry van der Schalie, whose touching obituary
is included in this number of The Nautilus. -R.T. A., editor].
To Joe Rosewater— from R. Tucker Abbott
[read at the 1985 memorial tribute at the
Smithsonian Institution]
The corridors of malacology may be darkened
today with the passing of our colleague and
friend, Joe Rosewater, but we and generations
to follow will find many bright rooms off to the
side that are filled with Joe's warm kindness and
illuminating scientific labors.
Calliostoma rosewateri- one of the most beau-
tiful seashells of the Caribbean - was appropri-
ately named after Joe by Drs. Clench and
Turner twenty five years ago. Joe loved and
understood the human qualities of his colleagues
and a year later, in his famous biography of
Calvin Goodrich, he quoted two letters written
to his mentor, Bill Clench:
"Thank you for naming the new species for
me. In the days to come when the new genera-
tion rolls up its sleeves to undo the work of
this one, as this one is undoing that of [tax-
onomic] workers who thought they had done a
good, decent job, some one will note the name
and speculate a bit about the guy it honors,
and that will be in the nature of fame."
And Joe, with a sense of humor, went on to
quote another prophetic letter:
"Your students [meaning Clench's students]
are of a high order. I was delighted with them,
and would steal them away if I knew just how
to go about it. After all, you've more students
than you should have, considering the rarity of
boys interested in mollusks. I wish you would
tell them that I consider it far more of a
pleasure to have met them and I have
delighted in their friendliness and intelli-
gence, whatever the police may think of
them."
Just a month ago I received a letter from a
now-retired, U. S. National Museum paleon-
tologist living in Florida:
"Joe really did a fine job of running the Divi-
sion of Mollusks, and one could always write
to him for help and expect a prompt reply. Joe
was a careful and meticulous researcher as
you well know."
Joseph Rosewater was born in Claremont,
New Hampshire, on September 18, 1928. He
was of the same New England breed of mala-
cologists as the Binneys, Dall, Morse, C. B.
Adams, A. E. Verrill and W. J. Clench. Follow-
ing his early college days at the University of
New Hampshire, Joe began his advanced train-
ing in malacology and museum curating at
Harvard University. He was a favorite student
of Clench's, and as Goodrich would say, was
unknown to the police.
His magnificent service to the Smithsonian In-
stitution began in 1960. Joe's twenty-five years
of malacology was a fulfillment of James
Smithson's bequest for the "increase and diffu-
sion of knowledge among all men." He served as
President of the American Malacological Union
in 1968, and as President of the National Capitol
Shell Club in 1964. His contributions to the
leading malacological journals of America are
well-known to his colleagues. His travels in
search of mollusks to the Marshall Islands,
Indonesia, Australia and Panama were the envy
of all devoted shell collectors. No more gentle
soul, with such a quiet sense of humor, nor with
a more natural ability to help both professional
or amateur malacologists could we all have
asked for. Let us hope that his successors will
match his sterling qualities. Let's light up the
halls of the National Museum once again.
About Bill Clench -from Mary C. Kline
[Mary Kline, now of Honolulu., and her late
husband, George, were for many years ardent
shell collectors who contributed many thousands
of specimens, photographs and much biological
Vol. 100(4)
October 31, 1986
THE NAUTILUS 153
information on motlusks for- the journals.
Johnsonia and Indo-Pacific Mollusca.]
Bill Clench was one of my favorite "ex-
tremists"-extremely kind, caring and loyal; an
extremely good raconteur. By his enthusiasm
for collecting shells and his insisting that the
neophyte keep good field notes, he directed
many beginners down the happy road to ex-
tremely rewarding and meaningful adventures.
Our friendship with Bill started about forty
years ago when George and I first fell prey to
the spell of the shell during a visit to Sanibel. On
that first day of beach-walking George found a
"different looking" shell. Local savants urged us
to write to Dr. Clench at Harvard. The shell
turned out to be an almost unheard of albino
Fasciolaria distans.
And so began an encouraging flood of corre-
spondence in response to our new shelling trips
to the Florida Keys and Bahamas. Bill was in
those days launching his new journal,
Johnsonia. We had many live-collected
specimens, plenty of notes and colored pictures
of animals. "Drop everything, come to the MCZ
[Museum of Comparative Zoology] for a week-
end and bring the slides." We went, we talked,
we spent a long time on the steps of the museum
bing innoculatead with Bill's enthusiasm. At his
home, his wife Julia, was a marvelous hostess
who had great patience and was a perfect house
mother to all and sundry who interested Bill.
Bill was many things but hardly the Ivory
Tower type. For example: one day when we ar-
rived at the museum lab he could hardly wait to
show us his latest treasure. We knew that he
and his associates had been working for a long
time on a seemingly endless project -cleaning
and rehabilitating the myriad drawers in the
many huge specimen cabinets. As each drawer
was finished a small blue star was affixed to the
front, indicating that it had been completed. At
last the goal had been reached and a party was
given to celebrate. Bill was presented with a
beautifully wrapped gift package. Inside was a
suitably framed miniature of a real pair of Long-
John bottoms with blue stars glued all over
them! How this wonderful man loved those
"Blue Starred Drawers!"
He begged us to become interested in land
shells as well as freshwater mollusks for, he
said, "the human population will grow and grow
and habitats will become neighborhoods -fresh-
water shells will disappear for pollution is in-
evitable but the sea will always be with us." He
lived to see the land fills where once there were
reefs. Many fashionable resorts now have
replaced sleepy lagoons over much of the
tropical world.
What did I learn from Bill? -so many things -
and here are just a few. 1 . A shell without data is
just a pretty bauble. 2. Learn the scientific
names, beach names are generally local. 3. Be
sure to learn the dangers of the areas in which
you are shelling -and avoid them. 4. Join the
A.M.U. and your local Shell Club. 5. In a foreign
country deal with the proper authorities and
remember, in your own way you represent
America. 6. Ask the museum curator how you
can help -leave the scientific side to him. 7.
Keep accurate notes and charts -be a good
observer. 8. Don't take all shells from one col-
ony-leave the habitat as you found it. 9. And
lastly, but far from least, keep your sense of
humor.
Remembering Bill Clench —
from Bunny Baker
[Mrs. Horace B. Baker, for many years the
business manager of The Nautilus, was raised
in Boston, and has been an ardent shelter for over
fifty years.]
I first met Bill Clench in the fall of 1933 when
I went to work at the Boston Children's
Museum. The museum's exhibits were mostly on
natural history topics, and though I was the
financial secretary and only office worker, I
thought I should know some natural history. My
lifelong friend and childhood chum, who also
worked in the museum, and I had collected
shells along the Mass. coast, and so that seemed
the logical place to start. I joined the Boston
Malacological Club, and there met Bill who was
to become a large part of my life.
In the fall of 1934 my chum, her mother, sister
and I went to Miami for our vacation. Her family
returned home by boat after a few days, and we
two girls drove across the Tamiami Trail to
Sanibel Island to collect shells. Bill had told us
so much about it that we wanted to collect there.
After a week we drove back to the east coast
and met Bill and two of his students who had
been on a collecting trip to Cuba. We all drove
154 THE NAUTILUS
October 31, 1986
Vol. 100(4)
down to Homestead and into the Everglades
where we camped out for five days and collected
Liguus. Bill helped us identify the various color
forms and taught us a lot about collecting and
cataloguing our catch. It was a wonderful ex-
perience and of course we all got really ac-
quainted with each other. We got hundreds of
shells, and those added to my Sanibel collection
and others from around the world gave me quite
a cabinetfull. They are now in Harvard's
Museum of Comparative Zoology.
Bill, his family and I saw much of each other; I
became Secretary-Treasurer of the Boston Club
and joined the A.M.U. It was at that meeting in
Toronto in 1939 that I met my husband. Bill in-
troduced us. In 1941 Bill drove his family and
me to the meeting in Rockland, Maine. After a
few days there I became engaged to H. B.
Baker. We were married in December, 1941,
and I moved to Philadelphia after a honeymoon
on Sanibel.
In subsequent years we saw Bill often and
kept in close touch. He had many friends and ad-
mirers. I am happy to have been one of them for
over 50 years.
We will never forget you, Bill.
To Bill -Cecelia W. Abbott
[Cecelia W. Abbott succeeded Mrs. Baker as
Business Manager of The Nautilus, and she often
accompanied Dr. Clench in his later Itfe on his
collecting trips to Kentucky, Georgia and
Florida and more recent A.M.U. meetings.]
So much of Bill Clench's life was devoted to
helping new students and encouraging
amateurs to study and collect shells that I
thought it only appropriate that a special trophy
be created for shell shows that would emphasize
his keen interest and love of land and fresh-
water mollusks.
The opportunity afforded itself when the
FIG. 1. Three proud winners of the William J. Clench Award
in Jacksonville, Florida, all of whom created outstanding ex-
hibits on non-marine mollusks. (from the left: Archie Jones,
Zida Kibler and Alfredo Romeu). Photo by William Kibler.
Jacksonville Shell Club celebrated its 25th anni-
versary in 1984. I lent a splendid sketch of Bill
and with the efforts and talents of club member,
Allan B. Walker, a handsome plaque was
designed. Bill's likeness, surmounted by two of
his favorite shells -Canthyri a spinosa (Lea) and
Triop.ns albolabris (Say) graced the William J.
Clench Award "to the outstanding exhibit of
land or freshwater mollusks that shows overall
excellence and best furthers interest in non-
marine conchology."
The award has now been given three times,
the first one, in 1984 to Archie Jones of Miami,
Florida, an old friend of Bill's and an expert on
Liguus. Other winners, to date, have been Zida
and William Kibler, in 1985, of Shallotte, North
Carolina, for their worldwide land shell exhibit,
and Dr. and Mrs. Alfredo Romeu of Jackson-
ville, Florida, for their Land Shell of the World
exhibit, 1986. Our hope has been realized that
this trophy is inspiring others to produce
outstanding, educational exhibits, and is
reminding us all of the wonderful qualities of
this kind and generous man after whom the
Clench Award is named.
0
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